Chemistry of the Environment [2nd ed] 0120734613, 978-0-12-073461-0

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Chemistry of the Environment by Sonja Krause, Herbert M. Clark, James P. Ferris, Robert L. Strong

•

ISBN: 0120734613

•

Pub. Date: March 2002

•

Publisher: Elsevier Science & Technology Books




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Table of Contents Preface About the Authors 1

Introduction

2

Atmospheric Composition and Behavior

3

Energy and Climate

4

Principles of Photochemistry

5

Atmospheric Photochemistry

6

Petroleum, Hydrocarbons, and Coal

7

Soaps, Synthetic Surfactants, and Polymers

8

Haloorganics and Pesticides

9

Chemistry in Aqueous Media The Environmental Chemistry of Some Important

10 Elements 11

Water Systems and Water Treatment

12

The Earth's Crust Properties and Reactions of Atomic Nuclei,

13 Radioactivity, and Ionizing Radiation

14

The Nuclear Environment

15

Energy

16

Solid Waste Disposal and Recycling

App. A

Designation of Spectroscopic States

App. B

Thorium and Actium Series

App. C

Units

App. D

Symbols and Abbreviations Index


INTRODUCTION



 Humans evolved on earth, with its atmosphere, land and water systems, and types of climate, in a way that permits us to cope reasonably well with this particular environment. Being intelligent and inquisitive, humans have not only investigated the environment extensively, but have done many things to change it. Other living things also change their environment; the roots of trees can crack rocks, and the herds of elephants in present-day African game parks are uprooting the trees and turning forests into grasslands. We are beginning to understand that microorganisms play a major role in determining the nature of our environment, not only through their actions on organic material, but also in systems traditionally regarded as strictly inorganicÐand not just at the earth's surface, but also at considerable depths. However, no other living things can change their environment in so many ways or as rapidly as humans. The possibility exists that we can change our environment into one that we cannot live in, just as the African elephant may be doing on a smaller scale. The elephants cannot learn to stop uprooting the trees they need for survival, but we should be capable of learning about our environment and about the problems we ourselves create.





      

One vital problem (among many) that we must solve is how to continue our technologically based civilization without at the same time irreversibly damaging the environment in which we evolved. This environment, which supports our life, is complex; the interrelations of its component parts are subtle and sometimes unexpected, and stress in one area may have far-reaching effects. This environment is also ®nite (hence the expression ``spaceship earth''). That being so, there is necessarily a limit before signi®cant environmental changes take place. Our modern technological society, coupled with largely uncontrolled population growth, places extreme stress on the environment, and many environmental problems come from prior failure to understand the nature of these stresses and to identify the limits. Many problems also come from refusal to accept that there are limits. Even for a component of our environment that is so large that for all practical purposes it can be taken as in®nite, such as the water in the oceans, there are limits. We cannot destroy a signi®cant amount of ocean water, but we can contaminate it. Many environmental problems and processes are chemical, and to understand them, understanding the basic chemistry involved is necessary (but not necessarily suf®cient). This is certainly true for those who wish to solve environmental problems, but also for those who need to make more general decisions that may have environmental consequences. It is important as well for those who would like to have some basis for understanding or evaluating the many, often contradictory, claims made regarding environmental problems. While the basic science underlying most environmental processes is well understood, many details are not. Too often, this lack of knowledge of the details of complex interactions is taken as an excuse to deny the validity of sound general conclusions, particularly when they run counter to political or religious dogma. In this book, we shall use the term ``environment'' to refer to the atmosphere±water±earth surroundings that make life possible; basically this is a physicochemical system. Our total environment consists also of cultural and aesthetic components, which we will not consider here. Neither shall we deal extensively with ecologyÐthat is, the interaction of living things with the environmentÐalthough some effects of the physicochemical system on life, and conversely, of living things on the physicochemical environment, will be included. Indeed, organisms play a major role in both organic and inorganic processes in the environment, and living things have made our environment what it is. Most obviously, the biological process of photosynthesis created the oxygen atmosphere in which we live.


       An immediate mental association with ``environment'' is ``pollution.'' Yet what constitutes a pollutant is not easily stated. One tends to associate the term with


    



materials produced by human activity that enter the environment with harmful effects especially on living organismsÐfor example, SO2 from combustion of sulfur-containing fuels, or hydrocarbons that contribute to smog. However, these and other ``pollutants'' would be present even in the absence of humans, sometimes in considerable amounts. We will consider a ``pollutant'' to be any substance not normally present, or present in larger concentrations than normal. One type of source commonly associated with pollution consists of industrial plants, especially chemical, but also factories using organic solvents, heavy metals, and so on. Another source is mining, including waste rock dumps and smelters. Waste disposal dumps are yet another source; materials can be released from these dumps. Military bases, training, and testing facilities may be sources of pollution from heavy metals as well as explosives residues. Fuel storage facilities, airports, and on a smaller but more widespread scale, gasoline stations may pollute through spills or leaking tanks. Power plants and incinerators may emit pollutants to the atmosphere, while automobiles and other internal combustion engines provide a delocalized but abundant source. Although any discussion of the environment must consider pollution, this will not be our primary aim. Rather, we will be concerned with some of the more important chemical principles that govern the behavior of the physicochemical environment and the interactions of its various facets. Among the controversial topics as this book is written are global warming and ozone depletion. The chemistry of these phenomena is discussed in some detail later in this book (Chapters 3 and 5), but an introduction to them at this point may give a useful illustration of environmental problems. With respect to global warming, some aspects are beyond scienti®c dispute, some are highly probable, and some are still uncertain. There is no question that introduction of carbon dioxide and some other gases into the atmosphere will increase heat retention, and that the atmospheric concentration of carbon dioxide has been increasing. It is also well established that introduction of some (but not all) particulate material into the upper atmosphere will re¯ect solar energy and lead to cooling. What is in question is how much of the introduced materials will be removed by natural processes, what the relative heating and cooling effects will be, and other details that need to be understood before a quantitative prediction of the net result can be made. It is almost certain that the average temperature of the earth's surface has increased in the last few years, and likely that at least part of this increase is due to human activity, but natural variabilty makes the latter conclusions less certain. Also uncertain are collateral changes in atmospheric circulation, rainfall, and ocean currents that could accompany an increase in global average temperature. There are two primary responses to these uncertainties. One is the attitude that if there is any doubt, one can ignore the potential problem and continue business as usual. The other is to assume the worst and advocate




    

massive changes at once, whatever the costs involved. An intermediate response, ``Make the changes that have moderate cost but move in the right direction,'' is often overlooked. Ozone destruction in the stratosphere by chloro¯uorocarbons, as discussed in Chapter 5, was clearly shown to be inherent in the chemistry of the atmosphere long before its observed decrease caused responsive action to be taken. Even then, many people refused to accept that human activities could have a deleterious effect and used uncertainties in the details of the destruction mechanism to argue against the need for controls. Some still do. Other responses to environmental problems are to focus on potential bene®ts, which is a perfectly valid thing to do if all the implications are understood. For example, it has been pointed out that global warming may have bene®cial effects by permitting agricultural activity in the Arctic regions, but do the soils in these regions have the necessary characteristics to support domestic plant growth? Will the possible increase in productivity in the Arctic balance possible losses elsewhere? What about changes in patterns of precipitation that may accompany temperature changes? It is also pointed out that massive environmental changes, including higher temperatures, have occurred naturally, so that anthropogenic changes do not involve anything new. This ignores the rate of change: changes that human activity can bring about may take place much more rapidly than those arising from natural causes, although knowledge of details is generally inadequate to predict time scales. For example, people could adjust to the conversion of, say, Wisconsin or Provence to a desert over a thousand years, but the same change in a few decades would be disastrous to the people involved. Two human activities that are strongly connected with environmental chemistry in general and pollution in particular are energy production and waste disposal, as discussed in Chapters 15 and 16, respectively. Aspects of the chemistry of these activities will be considered later, but some general comments are given here.


     Waste disposal is a growing problem. The environmental system consists of a very large amount of material: about 5
1018 kg of air and about 1
5
1018 m3 of water. In principle, comparatively large amounts of other materials can be dispersed in these, and consequently both the atmosphere and water bodies have long been used for disposal of wastes. This is sometimes done directly, and sometimes after partial degradation such as by incineration. In part, such disposal is based on the principle of dilution: when the waste material is suf®ciently dilute, it is not noticeable and perhaps not even detectable. A variety of chemical and biological reactions may also intervene to


    



change such input into normal environmental constituents (e.g., the chemical degradation of organic materials to CO2 and H2 O). Such disposal-by-dilution methods are not necessarily harmful in principle, but several factors must be considered in practice. The ®rst is the problem of mixing. While the eventual dilution of a given material may be acceptable, local concentrations may be quite high because mixing is far from instantaneous. As the disposal of wastes from more sources becomes necessary because of population or industrial growth in a particular area, it becomes more dif®cult to avoid undesirable local excess either continuously or as natural mixing conditions go through inef®cient periods. A second factor of long-term importance is the rate of degradation of waste material. It is obvious that if the rate of removal of any substance from a given sector of the environment remains slower than its rate of input, then the concentration of that material will eventually build up to an undesirable level. This is the case with many modern chemical products, including some pesticides and plastics that are only very slowly broken down into normal environmental components or rendered inaccessible by being trapped in sediments. Global contamination by such materials results from the dilution and mixing processes, and concentration levels increase while input continues. The examples of DDT and PCBs, discussed in Chapter 8, are well known. Other examples, such as the occurrence of pellets of plastics in signi®cant amounts even in the open ocean, may ultimately be of equal concern. There is also the problem of natural concentration. It is well known that some toxic materials (e.g., DDT and mercury) are concentrated in the food chain as they are absorbed from one organism to another without being excreted. Some plants can concentrate toxic materials from the soil. A third problem in disposal by dilution is the question of what concentration must be reached before harmful effects are produced. This is often dif®cult to answer, both because deleterious effects may be slow to develop and noticeable only statistically on large samples, and because often concentrations less than the parts-per-million range have to be considered. This is very low indeed, and often methods of detection and measurement become limiting in establishing the role of a particular substance. Finally, synergistic effects may come into playÐthat is, two or more substances existing at concentrations that separately are below the limits that are harmful may have highly deleterious effects when present together. Disposal by burying is a process that does not depend on dilution. In general, however, it ultimately depends either on degradation to harmless materials, or alternatively on the hope that the material stays put. Such considerations are particularly important with highly toxic or radioactive waste materials. Leaching of harmful components from such disposal sites and consequent contamination of groundwater or extraction from soils and concentration in plants are obvious concerns associated with such disposal methods.




 

Disposal of insoluble materials in the oceans also depends upon the principle of isolation of the waste. Solid materials may be attacked by seawater, and harmful components leached out into the water, ultimately to enter the food chain. Barrels or other containers for liquid wastes may corrode and leak. Contamination of the biological environment is a possible result. Ocean currents may play a role in distributing such wastes in unforeseen ways, as with New York City sewage sludge dumped in the Atlantic Ocean that migrated a long way from its dump site into adjacent waters. An extreme example of this occurred in 1995, when 4500 incendiary bombs washed up on Scottish beaches, injuring a child.1 These devices were believed to have come from the disturbance of an ocean dump of surplus munitions from World War II, dumped 10 km offshore in 1945, although the site had been used for munitions disposal from the 1920s up to the 1970s. Seven hundred antitank grenades and other weapons have washed up on beaches on the Isle of Man and Ireland from similar disposal sites. Clearly, understanding of a disposal problem involves knowledge of physical processes such as mixing, chemical processes involved in degradation reactions, chemical reactions of the waste and its products with various aspects of the environment, and biological processes, meteorological processes, geology, oceanography, and so on.


  The question of what constitutes a hazardous level of somethingÐfor example, radiation or a chemical that is carcinogenic or mutagenicÐis not easily answered. In part this is because years may pass before the consequences become identi®able. Even for materials with a more immediate effect, establishment of toxic levels may be problematic if the effects are not highly speci®c. Moreover, individuals vary in response, and the same responses may be due to alternate causes. Data on hazardous exposure levels could be obtained from epidemiological studies on large groups of people, but this would require the exposure of people to conditions known to be harmful. Experimental studies must use other species than humans, with the accompanying problems of species speci®city because of differing metabolisms, for example. (With our current knowledge, computer modeling or extrapolation from tests on simple organisms is not suf®cient, although such exercises may be helpful.) To make the scale of such experiments reasonable, usually small numbers of individuals are tested at high levels of dose, and results extrapolated to lower levels to get an estimate of risk for low levels of exposure. Past practice has generally been to use a linear extrapolation, implicitly assuming that there is zero effect only 1

R. Edwards,
 ., pp. 16±17, Nov. 18, 1995.


    



at zero concentration or exposure. Hence we had in the United States the Delaney clause prohibiting any detectable level of a carcinogenic additive in any food. There is abundant evidence, however, that organisms are often able to avoid or repair damage from substances up to a limit; that is, a threshold exists for many harmful effects, though that limit may be dif®cult to establish. Even when hazardous levels can be identi®ed, these are statistical; not all members of the exposed population will react the same way. Regulations designed to protect the public from exposure to harmful levels of substances involve some level of balance between cost and risk, although this practice may not be acknowledged explicitly at the time. Intelligent decisions about what this level should be involve many considerations, are often controversial, and are beyond the scope of this book.


  Energy production is a major activity of modern society that causes many environmental problems. Some of these problems are associated with the acquisition of the energy source itself (e.g., acid drainage from coal mines as discussed in Chapter 10, oil spills as discussed in Chapter 6), others with the energy production step (e.g., combustion by-products such as CO, SO2 , partially burned hydrocarbons, and nitrogen oxides considered in Chapters 5 and 10), while still others arise from disposal of wastes (e.g., nuclear ®ssion products, as will be seen in Chapter 14). In any device depending on conversion of heat to mechanical energy, (e.g., a turbine) the fraction of the heat that can be so converted depends on the difference between the temperature at which the heat enters, and that at which it leaves the device, as will be seen in Chapter 15. Practical restrictions on these temperatures limit ef®ciency and result in waste heat that must be dissipated, because making the exhaust temperature equal to ambient temperatures is not practical. This leads to the problem of thermal pollution. Such ef®ciency considerations also lead to the desire for ever higher input temperatures (i.e., the temperature in the combustion chamber). This in itself can produce secondary pollution problems, such as enhanced generation of nitrogen oxides.


    Basic to many environmental problems is the problem of human populationÐ its growth and the capacity of the earth to support it. Figure 1-1 shows the estimated human population from prehistoric times. Human population has increased by a factor of 4 from 1860 to 1961, while use of energy (other than




   

8

8

Modern Age

7

5

Old Stone Age

New Stone Age Commences

New Stone Age

Bronze Age

Iron Age

6

Middle Ages

4

5 4

Black Death - The Plague

Population (billions)

6

3

2 1

2.5 million 7000 B.C. years

6000

5000

4000

3000

2000

1000

B.C.

B.C.

B.C.

B.C.

B.C.

B.C.

A.D.

7

3

2 1

1000

2025

A.D.

A.D.

 

Human population trends from prehistoric times. Redrawn from         
   Copyright # 1994. Used by permission of the Population Reference Bureau.

human or animal power) increased more than 90-fold. This increase was accompanied by major increases in other resource needs as the technological base of society underwent drastic changes. Changes in resource use have not been uniform; a small fraction of the world's people, those in the developed nations, use most of the resources, although often these are obtained from lesser developed regions where the impact from mining, logging, and so on can be severe on local residents with little economic or political power to mitigate it. At the current rate of increase, 1.6% annually, the population will have doubled by the middle of the 21st century.2 Many factors make predictions of the actual increase unreliable (a prediction from the U.S. Bureau of the Census is shown in Figure 1-2), but certainly the numbers are such that one must consider what the effective carrying capacity of the earth is. This also is hard to evaluate3; it depends upon the lifestyle assumed, and on technological 2 Population increase is not uniform worldwide. Many industrialized nations have birthrates near or even below the replacement value, whereas population growth is largest in many of the least developed nations. The environment is deteriorating most severely in these less developed areas not from technological and industrial wastes and by-products, although these are increasing rapidly, but through environmental destruction driven by the needs of survival (e,g., deforestation in an effort to get ®rewood for cooking or to get land for growing food) or economic development. 3 J. E. Cohen, , 269, 341 (1995).


    

10 9

Population (billions)

8 7 6 5 4

3 2 1

1950

1960

1970

1980

1990

2000

2010

2020

2030

2040

2050

Year

 
 World population from 1950, projected to 2050. From U.S. Bureau of the Census, International Data Base.

solutions that may be developed for supplying food and other resources. Reliance on technological solutions yet to be developed to compensate for excessive population growthÐwhich is the only alternative to population control if we are to maintain any reasonable standard of livingÐseems to be a dangerous act of faith in view of the consequences of the failure of workable solutions to materialize. Optimists point to increased crop yields per acre and to the increase in total food production without an increase in the land area harvested in arguing that technology will be able to keep pace with population growth. Even so, the food so produced is often not available to people who need it. It is also pointed out that most processes, including food and energy production, are not carried out, on average, close to the ef®ciency already demonstrated in the best operations, and far from the ef®ciency that is possible in principle. Thus, it can be argued that even with current technology, an increased population, and increased productivity to support it, are possible without increasing our impact on the environment. On the other hand, considering the uneven distributions of resources and population, and normal human tendencies for short-term self-interest, one can have little con®dence that local disasters will be avoided.


"


 !    !   ! 

All predictions of the effects of continued population growth and related activities based on extrapolation of existing conditions are rendered questionable because of the complicated interrelationships among environmental factors, and also by the increasing recognition that there is not always a linear relationship between the factors that in¯uence a phenomenon and the level of the phenomenon itself. It has been proposed that many things, ranging from the spread of epidemics to the crime rate, exhibit a point of criticality: under a certain range of conditions, changes in the parameters that affect the phenomenon in question cause relatively proportional changes in it, but as these parameters approach some limiting values, small parameter changes begin to have very large effects. Is there such a critical point in the population±environment relationship? No one knows. Failure to account for nonlinear response to system perturbations is a major dif®culty in understanding or predicting environmental consequences in many areas.


 !    !   !  Almost everything that happens in the world around us could come under the general heading ``chemistry of the environment.'' Chemical reactions of all kinds occur continuously in the atmosphere, in oceans, lakes, and rivers, in all living things, and even underneath the earth's crust. These reactions take place quite independently of human activities. The latter serve to complicate an already complex subject. To understand environmental problems, we must have knowledge not only of what materials are being deliberately or inadvertently released into the environment, but also of the processes they then undergo. More than this, we need to understand the general principles underlying these processes so that reasonable predictions can be made about the effects to be expected from new but related substances. We must also understand the principles that underlie natural environmental processes to anticipate human interferences. This chemistry-oriented book emphasizes the chemical principles underlying environmental processes and the chemistry of the anthropogenic componentsÐthe materials and changes that humans have introduced. But to put these into context, some topics that are rather distant from reactions and equations need to be discussedÐas has been done in this chapter. In addition, knowledge in biological, meteorological, oceanographic, and other ®elds is equally important to the overall understanding of the environment. Indeed, although it is convenient to segment topics for study purposes, Barry Commoner's ®rst law of the environment should always be kept in mind: ``Everything is related to everything else.''


    





##$%$&'() *(#$'+ Alloway, B. J., and D. C. Ayres,       

, 2nd ed. Blackie, London, 1997. Bunce, N. J.,    , 3rd ed. Wuerz Publishing, Winnipeg, 1998. Brown, L. R., and H. Kane, 

 !"   #  "  , Norton, New York, 1994. Manahan, S. E.,    , 5th ed. Lewis Publishers, Chelsea, MI, 1991. O'Neill, P.,    , 2nd ed. Chapman & Hall, London, 1993.

2 ATMOSPHERIC COMPOSITION AND BEHAVIOR

2.1 INTRODUCTION There has been much discussion, both nationally and internationally, about the effects of various atmospheric pollutants on the earth's climate and on the earth's atmosphere. The United Nations Intergovernmental Panel on Climate Change (IPCC) report, data from the Goddard Space Science center of NASA, for example, shows that average global air temperatures have risen 0.6 to 0.78C over the last century (Figure 2-1). The 1997 Kyoto Protocol is an agreement among more than 150 countries to attempt to limit global warming by putting limits on their emission of carbon dioxide and some other greenhouse gases (see Section 3.3.3) to limit global warming. Furthermore, other international treaties including the Montreal Protocol of 1988 and its amendments limit and even ban the use of chloro¯uorocarbons and and the so-called halons in the United States and other countries at different times in order to stop the spread of the ``ozone holes'' in the stratosphere over the Arctic and Antarctic regions of the globe (see Section 5.2.3.5: Control of Ozone-Depleting Substances). Newspaper and magazine articles often make 13

14

2.1 INTRODUCTION

0.8 Global temperature (meteorological stations)

Temperature anomaly (⬚C)

0.6

0.4

0.2

0.0

−0.2

Annual mean 5-year mean

−0.4

−0.6 1880

1900

1920

1940

1960

1980

2000

Year FIGURE 2-1 Near-global annual mean surface air temperature from 1880 to 1998 relative to the mean surface air temperature between 1951 and 1980 (
148C). Data from the NASA Goddard Institute for Space Studies web site: http:==www.giss.nasa.gov.

these problems seem relatively simple but, in fact, they raise a number of questions: 1. What criteria are used to tell us that the earth's climate is becoming warmer? How do we take account of the normal year-to-year variability of the climate in any one area on the earth's surface? 2. Assuming that the criteria for de®ning the stated changes in the earth's climate are sound, how do these twentieth-century climate changes compare with other variations in climate noted in historic and prehistoric times? In other words, is there a possibility that the climate changes noticed during the latter half of the twentieth century are due, at least partially, to natural causes? Computer models (see Section 3.3.5) detailing the in¯uences of different factors on the earth's climate are being developed and may help answer this question. 3. Why should an increase in the carbon dioxide content of the atmosphere lead to a warming trend in the earth's climate? What other factors regulate the earth's climate?

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

15

4. What do we know about the general circulation of the atmosphere? After all, carbon dioxide and chloro¯uorocarbons are released into the atmosphere at particular locations on the earth's surface. How far do they spread through the atmosphere? 5. Although the carbon dioxide released into the atmosphere is said to affect the total climate, the macroclimate, of the earth, we humans actually live in small areas where we worry about microclimate. What do we know, for example, about the special climates of cities as opposed to their surrounding countrysides? How do the pollutants produced by human activities in cities become trapped in the atmosphere above these cities, to become hazards to people's health? We shall attempt to answer these questions in this and the following chapter, though not necessarily in the order in which they have been presented. The answers to most of these questions are complex and, in many cases, incomplete. It will thus be seen that questions and answers concerning the atmosphere and human effects on the atmosphere and climate are not simple and need a great deal of further study. This does not mean that action should not be taken, but it demonstrates the reason for the controversy surrounding these topics.

2.2 GASEOUS CONSTITUENTS OF THE ATMOSPHERE Table 2-1 shows the constituents of clean, dry air near sea level. Usually, the atmosphere also contains water vapor and dust, but these occur in amounts that vary widely from place to place and from time to time. Carbon dioxide, the fourth constituent on the list, has, as we shall see, been increasing in concentration during this century, mostly through the burning of fossil fuels such as coal and petroleum products. The concentrations given in Table 2-1 are estimated global averages for 1989; some of the trace constituents, like methane, have also been increasing in concentration, as noted later (see Section 3.3.3 and Figure 3-14). Trace constituents may vary in concentration in different parts of the atmosphere and in different parts of the globe. This is because many of these trace constituents are produced by different human and natural sources in different locations and are then removed from the atmosphere in different ways and by different means. For example, nitrogen oxides may be produced not only from human activities such as combustion in air but also from natural occurrences such as lightning discharges through the nitrogen and oxygen of the atmosphere and some photochemical reactions in the upper atmosphere (see Chapter 5, Section 5.2.1). Sulfur compounds arise not only from the combustion of sulfur-containing fuels but also from volcanic action. Methane

16

2.2 GASEOUS CONSTITUENTS OF THE ATMOSPHERE

TABLE 2-1 Some Constituents of Particulate-Free Dry Air near Sea Level Component N2 O2 Ar CO2 Ne CH4 Kr H2 N2 O H2 CO Xe O3 NO2 NH3 SO2 CH3 Cl CF2 Cl2 CFCl3 C2 H4 H2 S CCl4 CH3 CCl3

Volume (%) 78.084 20.948 0.934 0.0350 0.00182 0.00017 0.00011 0.00005 0.00003 0.00005 0.00001 9  106 110 106 2  106 6  107 2  107 5  108 4  108 2  108 2  108 1  108 1  108 1  108

generally comes from decaying organic matter while ammonia, H2 S, and some of the N2 O arise from decomposition of proteins by bacteria. The concentration of ozone, given in Table 2-1 at sea level, varies a great deal with altitude and somewhat with latitude. Section 2.5 discusses ozone concentration in greater detail. Although oxygen is a very reactive gas, its concentration is presently constant in our atmosphere; this implies a dynamic equilibrium involving atmospheric oxygen. It is well known that photosynthesis in green plants adds large amounts of oxygen to the atmosphere during daylight hours. Although oxygen may also be produced in other ways, the amounts are much smaller than those produced by photosynthesis. It seems reasonable to suppose that the oxygen produced by photosynthesis makes up for the equally vast amounts of oxygen used up by the respiration of plants and animals, by weathering of rocks, by burning of fossil fuels, and by other oxidative processes that take place in the atmosphere. This balance, however, requires green plants that were

17

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

CO2 concentration (ppm by volume)

380

360

340

320

300

280

260 1700

1750

1800

1850 Year

1900

1950

2000

FIGURE 2-2 Historical variation of carbon dioxide in the atmosphere from 1744 through 1999. Data from the U.S. National Oceanic and Atmospheric Administration (NOAA) Climate Monitoring and Diagnosis Laboratory (CMDL), Carbon Cycle±Greenhouse Gases Branch; antarctic ice core samples and atmospheric measurements. http:==www.cmdl.noaa.gov.

not present in the very distant past. The various theories that describe the earth as evolving from a primordial, lifeless state to its present condition, and the physical evidence that supports these theories, suggest that little or no oxygen was present on the primordial earth. Carbon dioxide has been released into the atmosphere in signi®cant amounts since the beginning of the industrial age through the burning of fossil fuels.1 Furthermore, the destruction of forests in the tropics and temperate regions of the earth has reduced the removal of CO2 from the atmosphere by green plants. Studies of carbon dioxide in ice cores from both Greenland and Antarctica have shown a large variability in the concentration of CO2 in the atmosphere over the past 160,000 years (see Figure 3-13), but in more recent times it was about 280 ppm from 500 b . c . to about a . d . 1790. Figure 2-2 shows the average CO2 concentration in the atmosphere from 1744 to 2000 as estimated from measurements made on Antarctic ice cores and in the atmosphere. Measurements made in the atmosphere at Mauna Loa, Hawaii, indicate that the average concentration of CO2 was 315 ppm by 1958 and about 370 ppm by 2000. Figure 2-3 shows the data obtained at Mauna Loa between 1

The carbon cycle, which includes carbon dioxide, is discussed in greater detail in Section 10.2.

18

2.2 GASEOUS CONSTITUENTS OF THE ATMOSPHERE

380 370

CO2 (ppm)

360 350 340 330 320 310 1955

1965

1975

1985

1995

2005

Year FIGURE 2-3 Monthly variation of atmospheric concentrations of carbon dioxide at Mauna Loa Observatory. Data prior to May 1974 are from the Scripps Institution of Oceanography; data since May 1974 are from the National Oceanic and Atmospheric Administration, Climate Monitoring and Diagnosis Laboratory Carbon Cycle±Greenhouse Gases Branch. http:==www.cmdl.noaa.gov.

1958 and 2000. Mauna Loa is situated at a latitude of approximately 198N. Note that there are seasonal variations in the carbon dioxide content of the atmosphere over Mauna Loa: less CO2 is found in the summer, the growing season in the Northern Hemisphere. Hawaii may seem rather far south to feel the effects of this; more northerly areas like Scandinavia and northern Alaska show seasonal variations that have twice the amplitude of those over Mauna Loa. Seasonal variations in CO2 concentration in the Southern hemisphere are much smaller. At present, about 1:9  1010 metric tons of ``new'' CO2 are released into the atmosphere every year, mostly from the burning of fossil fuels; this is estimated to be about 10% of the amount used by green plants in the same time. About 47% of this new CO2 is absorbed by the oceans rather quickly; given enough time, it is possible that the oceans would absorb much more. More details on the distribution of CO2 in nature and on the carbon cycle in general are given in Section 10.2. At this time, the atmospheric concentration of CO2 appears to be increasing at the rate of 1.3 ppm per year. The possible effects of this increase on the earth's climate are discussed in Chapter 3.

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

19

Carbon monoxide as well as CO2 is released to the atmosphere by the burning of fossil fuels, and also by volcanic and biological activity. It is possible that carbon monoxide is accumulating in the atmosphere above the Northern Hemisphere at this time, but the data are too variable for de®nitive conclusions. It is known, however, that carbon monoxide cannot be accumulating as rapidly as it is emitted into the atmosphere, and thus there has been much interest in the origin and fate of atmospheric CO. It appears that about 50% of the carbon monoxide entering the atmosphere each year comes from natural processes. Estimates of carbon monoxide entering the atmosphere each year made since 1990 are as follows: over 109 metric tons from natural causes such as the oxidation of methane arising from the decay of organic matter, the biosynthesis and degradation of chlorophyll, and release from the oceans, and over 109 metric tons from human activities. These ®gures indicate that removal of CO from the atmosphere must be occurring with great ef®ciency. Carbon monoxide reacts with hydroxyl radicals in the lower atmosphere (see Section 5.3.2), and there is evidence that fungi and some bacteria in the soil can utilize CO, converting it to CO2 . However, because of its toxicity, CO can be a major problem in areas in which its concentration is elevated. For example, although the worldwide concentration of CO varies between 0.1 and 0.5 ppm, its concentration in the air over large cities can be 50±100 times as great, up to 50 ppm. It has been dif®cult to quantify the toxic effects on humans due to the CO in the atmosphere above large cities because the CO concentration in automobiles in heavy traf®c can be much higher and because smokers inhale large quantities of CO. However, in one study2 it was shown that 20.2 ppm of CO above Los Angeles County in 1962±1965 resulted in 11 more deaths per day than occurred when the CO concentration was 7.3 ppm. Sulfur and nitrogen compounds in the atmosphere are discussed at greater length in Chapter 10. At this point, we shall simply say that the sulfur compounds (mostly SO2 ) that arise from the burning of fossil fuels come back to earth in the form of sulfuric acid dissolved in rainwater after undergoing further oxidation in the atmosphere (see Chapter 5). Some of the nitrogen oxides also dissolve in rainwater to form acids. Normal rainwater, which always contains CO2 as well as some naturally occurring acids, may have a pH as low as 5.0 (see Section 11.4). In the last 50 years, however, rain and snow of much lower pH, that is, higher acidity, has been reported from many parts of the world. Rainfall in the northeastern United States now usually has a pH between 4.0 and 4.2, but individual rainstorms may have a pH as low as 2.1. Major industrial sources of atmospheric sulfur compounds are generally situated upwind of areas that have acid rain, and individual storms that have rain with very low pH have usually passed over large sources 2

A. C. Hexter and J. R. Goldsmith, Science, 172, 265 (1971).

20

2.3 HISTORY OF THE ATMOSPHERE

of these compounds. Tracer experiments, in which a marker gas such as sulfur hexa¯uoride has been injected into a waste gas stream from a chimney and followed by an aircraft containing appropriate instrumentation, have shown that such gases do not disperse where they ®rst appear but move with the prevailing winds. For example, gases released from the east coast of England have been followed to Scandinavia. The Scandinavian countries, which are downwind not only from England but also from Germany's heavily industrialized Ruhr Valley, have had rain with pH as low as 2.8. Even in South America's Amazon Basin, with very little nearby industrial activity, pH values as low as 4 have been recorded. Acid rains in Europe and elsewhere have led to rapid weathering of ancient structures and sculptures during the latter half of this century; some of these structures, such as the Parthenon in Athens, had stood virtually unchanged for hundreds and, in some cases thousands of years. Some of the chemistry involved is discussed in Section 9.2.2. In Germany and elsewhere, ancient forests are dying, presumably because of acid rain. The effects of acid rain on lakes, running waters, and ®sh are described in Section 11.4. Methane is a trace gas that has received considerable attention in recent years. Studies of Antarctic ice cores indicate that the atmospheric methane concentration was as variable as the carbon dioxide concentration over the past 160,000 years (see Figure 3-13). However, from 25,000 b . c . to a . d . 1580, the methane content of the atmosphere was approximately constant; it began increasing at that time up to the present value of about 1.75 ppm. This increase was as large as 0.016 ppm=year in 1991; with some large oscillations, this rate of increase has dropped between 1991 and 1999. Natural sources of methane include anaerobic bacterial fermentation in wetlands and intestinal fermentation in mammals and insects such as termites, and these account for most of the methane entering the atmosphere. The ``sinks'' for atmospheric methane are not well understood, and the impact of human activities on methane formation and destruction has not been ascertained. The increase in methane content of the atmosphere can have important consequences for the earth's climate (see Section 3.3.3).

2.3 HISTORY OF THE ATMOSPHERE 2.3.1 Evidence and General Theory Unfortunately, there is no agreement in the literature either on the composition or on the time of origin of the earth's original atmosphere. Evidence for the composition of the atmosphere at earlier times comes from a study of objects that were formed in contact with the atmosphere at those times. These objects may have changed since, but they still provide us with clues about

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

21

the conditions existing when they were formed. The earliest such objects in existence are sedimentary rocks about 3  109 years old. It is believed that these rocks could not have been formed without prior atmospheric weathering, or without large amounts of liquid water. Therefore, water was probably present in the primitive atmosphere. On the other hand, the compositions of these and later rocks indicate that the atmosphere could not have contained much oxygen before 18  109 years ago. Also, the relative rarity of carbonate rocks such as limestone and dolomite among the oldest sedimentary rocks seems to indicate that bases such as ammonia cannot have been abundant in the primitive atmosphere. The presence of ammonia would have increased the pH of the primitive ocean and thus favored an abundance of carbonate rocks (see Chapter 9). Furthermore, in the absence of atmospheric oxygen and ozone, methane and ammonia would be rapidly dissociated after absorbing high-energy ultraviolet radiation. In this chapter, therefore, we shall assume the absence of large amounts of CH4 and NH3 from the primitive atmosphere. According to another school of thought, however, CH4 and NH3 must have been present in the primitive atmosphere, and evidence presented thus for for their absence has been insuf®cient. Moreover, experiments have been performed to show that an atmosphere dominated by CH4 and NH3 would be suitable for the evolution of complex organic molecules. Discussion of these con¯icting viewpoints is beyond the scope of this book. A combination of the geologic record and the present composition of the atmosphere, along with some reasonable conjectures, leads to the conclusion that the primitive atmosphere probably contained N2 , H2 O, and CO2 in approximately their present amounts plus a small percentage of H2 and a trace of oxygen. Volcanic gases contain H2 O, CO2 , SO2 , N2 , H2 , CO, S2 , H2 S, Cl2 , and other components. Of these, H2 O is the most abundant, followed by CO2 and SO2 or H2 S, depending on the volcano. Presumably, in the distant past, there was more volcanic action and thus the earth degassed somewhat faster than at present. The rate of ``degassing'' of the earth has varied throughout its history. The earth at present is emitting mostly water vapor and carbon dioxide, some nitrogen and other gases, and no oxygen. These data must be reconciled with the composition of the atmosphere as given in Table 2-1. Calculations3 indicate that the total quantity of water vapor released by the earth over all time is about 3  105 g=cm2 averaged over all the earth's surface. Most of this water vapor has condensed and is presently in lakes and oceans. The oxygen now present in the atmosphere has probably arisen from photosynthesis after the evolution of green plants. 3

F. S. Johnson in S. F., Singer, ed., Global Effects of Environmental Pollution. Springer-Verlag, New York, 1970.

22

2.3 HISTORY OF THE ATMOSPHERE

2.3.2 Carbon Dioxide Carbon dioxide has been emitted to the extent of about 5  104 g=cm2 of the earth's surface over all time. Most of this CO2 has dissolved in the oceans and much has precipitated from the oceans as calcium carbonate. Only about 0:45 g=cm2 CO2 remains in the atmosphere, while about 27 g=cm2 averaged over all the earth's surface is dissolved in the oceans. There is 60 times as much CO2 dissolved in the oceans as there is free in the atmosphere, but most of the carbon dioxide released by the degassing of the earth is now tied up in geologic deposits (i.e., carbonate rocks). There are complex equilibria, discussed in Chapter 9, between the atmospheric CO2 and that dissolved in the oceans. Recent experiments have shown that it takes about 470 days to dissolve half the CO2 placed in contact with turbulent seawater. Complete equilibrium takes much longer, with estimates ranging from 5 to 500 years, but, given suf®cient time, the oceans and rocks act as an enormous sink for any CO2 that is added to the atmosphere. That is, most of the CO2 added to the atmosphere eventually ends up in the oceans and in geologic deposits. However, we are now adding CO2 to the atmosphere by burning fossil fuels in the amount of about 1:9  1010 metric tons per year (see Section 2.2); this adds to the 2:6  1012 metric tons of CO2 already present in the atmosphere. Some of the added CO2 will remain in the atmosphere even when atmosphere±ocean equilibrium has been achieved. The World Energy Council estimated that the amount of all recoverable fossil fuels was about 4:6  1012 metric tons4 in 1993. This would allow 1:9  1010 metric tons to be burned each year for over 300 years. However, the provisions of the Kyoto Protocol may limit the amount of fossil fuels burned in the future so that the earth's supplies could last much longer than 300 years. The concentration of carbon dioxide in the atmosphere in the nineteenth century was about 290 ppm, while in 2000, as mentioned in Section 2.2, it was about 370 ppm. The increased concentration in this century is well documented and will be discussed later, together with its possible effects on climate. Much carbon dioxide is used by green plants in photosynthesis, but this carbon dioxide is returned to the atmosphere by decay and oxidation in living things. Production of CO2 from fossil fuels uses atmospheric oxygen, but this has little effect on the oxygen content of the atmosphere. For example, if all easily recoverable fossil fuels were burned at once, calculations indicate that only 10% of the atmospheric oxygen (a total of 5  1014 metric tons) would be used up.

4

This is given in terms of the equivalent mass of petroleum, since fossil fuels include soft and hard coals as well as petroleum.

23

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

2.3.3 Nitrogen Compared with CO2 , relatively small amounts of nitrogen have been released by degassing of the earth, only about 103 g=cm2 of the earth's surface. But nitrogen is chemically inert, and at least 90% of this amount is still present in the atmosphere. The nitrogen no longer present in the atmosphere is mostly present in geologic deposits; the tiny fraction (108 ) of the available atmospheric nitrogen that is ``®xed'' each year is soon returned to the atmosphere when plants and animals decay. The nitrogen cycle is discussed more fully in Section 10.3.

2.3.4 Oxygen We have seen that atmospheric oxygen does not arise directly out of degassing of the earth but comes from photosynthesis in green plants and, possibly, from the photodissociation of water vapor in the upper atmosphere as shown in Equation 2-1. n

H2 O gH2 g  1=2O2 g

2-1

Thus, during the photodissociation of water vapor, hydrogen gas is produced as well as oxygen gas. Hydrogen molecules, being much less massive than other atmospheric gas molecules, have a higher speed than these molecules at any temperature anywhere in the atmosphere, and many have a velocity greater than the escape velocity from earth's gravitational ®eld. It has been calculated that hydrogen gas escapes at the rate of approximately 108 atoms=s per square centimeter of earth's surface. Over all time, about 1017 s, then, 1025 atoms=cm2 , about 17 g=cm2 , has escaped, which accounts for up to about 150 g=cm2 of dissociated water vapor. This number corresponds to about 0.05% of the total water vapor released during the degassing of the earth; however, some of the escaped hydrogen was probably of volcanic origin. Furthermore, there is controversy over whether enough water vapor is transported to the upper layers of the atmosphere to allow photodissociation to take place. The relative importance of photodissociation of water vapor versus photosynthesis is in dispute, with past estimates ranging from 100% photodissociation to 100% photosynthesis. In recent years, photosynthesis has been assumed to play the major role. In the present discussion, it is immaterial where all the oxygen now present in the atmosphere, in living things, and in oxidized rocks and minerals originated. At what rate did oxygen accumulate in the atmosphere? There is some fossil evidence that the ®rst anaerobic forms of life originated about 3:5  109 years

24

2.4 PARTICULATE CONSTITUENTS OF THE ATMOSPHERE

ago. These life-forms may have released some oxygen into the atmosphere, adding to that produced by the photodissociation of water vapor. About 1% of the present amount of oxygen had accumulated in the atmosphere 6  108 years ago. At this point, respiration could begin in living things, as well as, ozone formation in the upper atmosphere, as will be discussed in Section 2.5. The atmospheric ozone screens certain ultraviolet wavelengths completely from the surface of the earth at present. When the oxygen level had reached 1% of its present value, screening of these harmful wavelengths was suf®cient to permit the development of a variety of new life-forms in the oceans. By the start of the Silurian era, 42  108 years ago, the earth's oxygen level had reached about 10% of its present level, and suf®cient ozone was present in the upper atmosphere to allow life to evolve on land. Most of the oxygen that has been produced in all this time has been used up in the oxidation of rocks and other surface materials on earth. However, more oxygen is still being produced, both by photodissociation and by photosynthesis.

2.4 PARTICULATE CONSTITUENTS OF THE ATMOSPHERE Table 2-1 does not include the ``particulate matter,'' dust, or, in general, the nongaseous matter that is usually present in the atmosphere. These are particles, which are 107 102 cm in radius, that is, from approximately molecular dimensions to sizes that settle fairly rapidly. Particulate matter in the atmosphere can be natural or man-made. Table 2-2 gives some estimates of the tonnage of particles with radii less than 2  103 cm (20 mm) emitted to the atmosphere each year. Table 2-2 indicates that particles of human origin constitute between 5 and 45% of the total appearing in the atmosphere annually at the present time. Other estimates are as high as 60% These estimates cover a large range because some occurrences, like volcanic action, are inherently variable and because some of the other sources of particulate matter are very dif®cult to estimate. Large particles can settle out of the atmosphere by sedimentation in the earth's gravitational ®eld. Furthermore, it is estimated that approximately 70% of the particulate matter that enters the atmosphere is eventually rained back out, probably because the particles act as condensation nuclei for the water droplets that form rain clouds. The particles are accelerated by the gravitational force but retarded by friction with the gas molecules of the air, thus reaching a terminal sedimentation velocity which is related to the radius of each particle as shown in Table 2-3, which, by the way, refers to water droplets as well as particles. Water droplets with radii from 1 to 50 mm may be present in clouds, while droplets with radii of 100 mm generally fall as a drizzle. Larger droplets fall as rain.

25

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

TABLE 2-2 Estimate of Particles Emitted into or Formed in the Atmosphere Each Year Particle sources Natural Soil and rock debris Forest ®res and slash burning Sea salt Volcanic action Gaseous emissions Sulfate from H2 S NH 4 salts from NH3 Nitrate from NOx Hydrocarbons from vegetation Natural particle subtotal Human origin Direct emissions, smoke, etc. Gaseous emissions: Sulfate from SO2 Nitrate from NOx Hydrocarbons Human origin particle subtotal Grand total

Quantity (megatons=year)

100±500 3±150 300 25±150 130±200 80±270 60±430 75±200 773±2200 10±90 130±200 30±35 15±90 185±415 958±2615

Source: Reprinted, with some modi®cation, from Inadvertent Climate Modi®cation, Report on the Study of Man's Impact on Climate (SMIC), MIT Press, Cambridge, MA, 1971.

The smallest solid particles, many with radii of only 0.1±1.0 mm, have a maximum concentration about 18 km above the earth's surface. Some of these arise from volcanic eruptions, while others are particles of ammonium sulfate formed when H2 S and SO2 in the atmosphere are oxidized and the resulting

TABLE 2-3 Sedimentation Velocity of Particles with Density 1 g=cm3 in Still Air at 08C and 1 atm Pressure Radius of particle (mm) < 0:1 0.1 (105 cm) 1.0 10.0 100.0 (102 cm)

Sedimentation velocity (cm=s) Negligible 8  105 4  103 0.3 25

26

2.5 EXTENT OF THE ATMOSPHERE AND ITS TEMPERATURE AND PRESSURE PROFILE

H2 SO4 neutralized another atmospheric constituent, ammonia. The mean residence time of particulate matter in the lower atmosphere is between 3 and 22 days. In the stratosphere it is 6 months to 5 years, in the mesosphere from 5 to 10 years. (The meaning of ``stratosphere'' and ``mesosphere'' will be explained in the next section.) At any rate, the higher in the atmosphereÐthat is, the farther above the surface of the earth the particles have reachedÐthe longer it takes them to come down. Particles with radii from 0.02 to 10 mm may contribute to the turbidity of the atmosphere. We shall see later that the turbidity of the atmosphere is an important determinant of the earth's climate. The atmosphere has become more turbid over the past half-century, as shown by monitoring both in urban locations such as Washington, D.C., and in the mountains, such as Davos, Switzerland.

2.5 EXTENT OF THE ATMOSPHERE AND ITS TEMPERATURE AND PRESSURE PROFILE Roughly 51  1018 kg of atmosphere is distributed over the 51  1014 m2 of the earth's surface. This means that atmospheric pressure at sea level is about 104 kg=m2 , or 103 g=cm2 . This is approximately equivalent to one standard atmosphere of pressure (1013 mbar). Most of the atmosphere is fairly close to the surface of the earth. Fifty percent of the atmosphere is within 5 km (3 mi) of sea level, that is, at a height of somewhat more than 5 km above sea level, atmospheric pressure is 0.5 atm. There are quite a few mountains that are higher than this. One such mountain is Kilimanjaro in Tanzania, which rises nearly 6 km above sea level; Mount Whitney and the Matterhorn are just under 5 km in altitude. Ninety percent of the atmosphere is within 12 km of sea level. By comparing 12 km with the radius of the earth, 6370 km, it is seen that 90% of the atmosphere exists in an extremely thin layer covering the earth's surface. The total extent of the atmosphere is much harder to specify, since there is no de®nite upper boundary. For most purposes, one can say that the atmosphere ends between 200 and 400 km above the earth's surface, but on occasion it is necessary to consider a few hundred or a thousand additional kilometers. Nitrogen, oxygen, and carbon dioxide are reasonably well distributed at all altitudes in the atmosphere. Most of the water vapor and water droplets occur at altitudes below about 14 km, while most of the ozone is localized in the vicinity of 25 km above the earth's surface. There is, however, some water vapor at altitudes above 14 km, about 3 ppm in the stratosphere. The exact manner in which temperature and pressure change with altitude in the atmosphere depends both on latitude and on the season of the year. Very close to the surface of the earth, temperature and pressure are extremely

27

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

variable, even beyond the latitude and seasonal variations. For this reason, various national and international groups have proposed ``standard atmospheres'' at various times. For illustrative purposes (see Table 2-4), we shall use the U.S. Standard Atmosphere, 1962, which depicts idealized year-round mean conditions for middle latitudes such as 458N, for a range of solar activity that falls between sunspot minimum and sunspot maximum. Standard information for other latitudes and for various times of year can be found in the Additional Reading at the end of this chapter. Table 2-4 shows that the pressure drops off continuously with increasing altitude, but the temperature goes through some strange gyrations. The temperature of the atmosphere decreases from sea level TABLE 2-4 Temperature and Pressure of the Standard Atmosphere Altitude (km)

 (mbar)

T (K)

0 1 2 5 10

1013 899 795 540 265

288 (158C) 282 275 (28C) 256 223 (508C)

12 15 20

194 121 55

217 217 (568C) 217

25 30 40

25 12 3

222 227 250

50

0.8

271 (28C)

60 70

0.2 0.06

256 220

80 90

0.01 0.002

180 180 (938C)

100 110 120 130 140 150 175 200 300 400 500

0.0003 7  105 3  105 1  105 7  106 5  106 2  106 1  106 2  107 4  108 1  108

210 257 350 (778C) 534 714 893 (6208C) 1130 1236 1432 1487 1500 (12278C)

Source: Adapted from U.S. Standard Atmosphere, U.S. Government Printing Of®ce.

28

2.5 EXTENT OF THE ATMOSPHERE AND ITS TEMPERATURE AND PRESSURE PROFILE

10−7

Altitude (km)

Ionosphere (50– 4000 km)

10−6

200

Thermosphere (85– 500 km)

100

Mesopause

10−5 Auroras ice clouds

Mesosphere (50– 85 km) Stratopause

Meteors burn O3 formed

Stratosphere Tropopause

0 100

200

300

500

Troposphere

(Weather)

Pressure (millilbars)

300

10−3

10−1 1 10 100 1000

1000 2000 Temperature (K)

FIGURE 2-4 Temperature and pressure pro®le of the U.S. Standard Atmosphere.

up to 12 km, remains constant up to 20 km (at least in the U.S. Standard Atmosphere, 1962), increases from 20 to 50 km, decreases again from 50 to 80 km, remains constant to 90 km, and then increases asymptotically to about 1500 K above 300 km. These variations are probably less confusing as depicted in Figure 2-4, which also shows the change in pressure with altitude. Note that the temperature scale in Figure 2-4 is logarithmic, to make it easier to see the temperature variations in the ®rst 100 km of the atmosphere. Starting at the earth's surface, at sea level, the temperature of the standard atmosphere decreases steadily in the troposphere (sometimes referred to as the lower atmosphere) up to the tropopause. We shall see in Chapter 3 how temperature inversions, (i.e., regions where the temperature increases with increasing altitude) can sometimes occur in the troposphere. The troposphere contains most of the mass of the atmosphere, it is the only continuously turbulent part of the atmosphere, and it contains most of our weather systems. Atmospheric pressure drops off logarithmically with altitude near the earth's surface, but more slowly at higher elevations, and there are no pressure inversions.5 5 The thermodynamic concept of an equilibrium temperature may not be valid at elevations above 350 km where the pressure is less than 107 mbar. The very few molecules present, seldom collide, and thus they probably are not at equilibrium. Thus, the temperature at altitudes above 300 km should be considered to be a mean kinetic temperature, having to do with the average kinetic energy of the molecules present.

29

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

Wherever the temperature rises with an increase in altitude in the atmosphere, there must be one or more exothermic (i.e., solar-energy-absorbing) chemical reactions involved. Without such processes, the temperature of the atmosphere would vary smoothly from warm at the earth's surface to very cold, close to absolute zero, at very high altitudes. Radiant energy from the sun is absorbed in various photochemical processes both in the stratosphere and in the thermosphere, thus increasing the temperature with increasing altitude as shown in Figure 2-4. The photochemical processes of the thermosphere will be fully discussed in Chapter 5. At this point, let us simply note that atmospheric oxygen and nitrogen in the thermosphere above 100 km absorb virtually all the ultraviolet radiation having wavelengths below 180 nm (1800 AÊ). This circumstance is very fortunate for two reasons. First, this high-energy radiation would initiate chemical reactions in all complex molecules, with the result that life as we know it would be impossible if this radiation reached the earth's surface. Second, the large variations in the intensity of the sun's radiation at these short wavelengths have very little effect on the troposphere where our weather originates, since all these wavelengths are removed at much higher altitudes. Radiation with wavelengths between 180 and 290 nm would also be destructive to life, but these wavelengths are absorbed in the stratosphere by oxygen and ozone. The maximum absorption of ozone is at 255 nm (see Section 5.2.3.1). The major reactions in the stratosphere, much simpli®ed from the more complete discussion to be found in Section 5.2.3.1, are as follows: n

O2 ƒ O  O

O2  O  M  O3  M

2-2 

n

O3 ƒ O2  O

O  O3  2O2  kinetic energy

2-3 2-4 2-5

Reaction (2-2) also occurs at higher altitudes, but does not lead to reaction (2-3) because the pressure is too low to allow termolecular collisions to occur with any reasonable frequency. A third atom or molecule M is needed for reaction (2-3), so that both energy and momentum can be conserved in the reaction. The symbol M* refers to the increase in the energy of M while O2 is combining with O to form O3 . Ozone is formed down to about 35 km altitude, below which the ultraviolet radiation necessary for its formation (l  240 nm) has been fully absorbed. Most of the ozone in the atmosphere, however, exists at altitudes between 15 and 35 km, so that mixing processes must occur in the stratosphere as well as in the troposphere. Also, ozone concentrations are low over the equator, where, on the average, most of the sun's radiation impinges, and high near

30

2.6 GENERAL CIRCULATION OF THE ATMOSPHERE

the poles, at latitudes greater than 508, where less radiation comes in from the sun. Consequently, it is obvious that there are mechanisms for the transport of ozone from the equator to the poles. Furthermore, there are transitory losses of ozone over the Antarctic and (sometimes) Arctic regions during their early springtimes (see Sections 5.2.3.3 and 5.2.3.4, respectively). This ozone appears to be replenished during the Antarctic summer by transport from the stratosphere over the temperate regions of the southern hemisphere. Transport of gases through the tropopause and from one region of the stratosphere to another occurs readily; this transport has seasonal aspects and the mechanism is quite complicated and is still being studied. Ê ) is transmitSolar radiation with wavelengths greater than 290 nm (2900 A ted to the lower stratosphere, the troposphere, and the earth's surface. We shall see that this remaining radiation, including UV with wavelengths exceeding 290 nm, visible and infrared, comprises more than 97% of the total energy from the sun.

2.6 GENERAL CIRCULATION OF THE ATMOSPHERE Only very general patterns of atmospheric movement are within the scope of this chapter, where they are pertinent because we are interested in discussing general movements of pollutants and other constituents of the atmosphere. Atmospheric circulation will thus be considered in an extremely simpli®ed manner. Books on meteorology, such as the ones given in the Additional Reading at the end of this chapter, may be consulted for further details. There are two major reasons for the existence of a general circulation of the atmosphere. First of all, the equatorial regions on earth receive much more solar energy all year round than the polar regions. Hot air therefore tends to move from the equator to the poles, while cold air tends to move from the poles toward the equator. As we shall see, the surface of the earth absorbs a much larger proportion of the solar radiation than the atmosphere above it. Thus, in the troposphere, the air is heated by conduction, convection, and radiation from the ground. There is also some heating of the atmosphere when water vapor, recently evaporated from the earth's surface, condenses to form clouds. If we recall that hot air is less dense than cold air and tends to rise above it (this will be discussed in Chapter 3 in connection with temperature inversions, Section 3.5), we shall expect hot air to rise near the equator and ¯ow toward the poles at some elevation above the surface of the earth. The colder air from the polar regions is then expected to ¯ow toward the equator nearer to the surface of the earth, as shown in Figure 2-5. This idea was ®rst formulated by G. Hadley in 1735. Hadley's picture of atmospheric circulation also took account of the earth's rotation, but for the moment we should note the

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

31

N

Equator

S

FIGURE 2-5 General circulation of the atmosphere as proposed by Hadley, 1735. These were the simplest forms of ``Hadley cells,'' with hot air rising near the equator and moving toward the poles in the upper troposphere. Cold air, in this model, moves from the poles toward the equator near the surface of the earth.

following major oversimpli®cations in his model. First, this model showed a lot of air accumulating over the polar regions; second, no account was taken of unequal heating of land and sea; and, third, no account was taken of variations in solar radiation at various latitudes at different times of the year. What happens when the rotation of the earth from west to east is taken into account? If we think of the earth as rotating around an axis that goes through the North and South Poles, we note that the surface of the earth at the poles does not rotate, while the surface of the earth at the equator rotates very quickly. The equatorial circumference of the earth is about 40,000 km, and one rotation occurs every 24 h, so that every point on the earth's equator is constantly moving at a velocity of 28 km=min in contrast to the stationary points at the poles. In the same way, the air above the poles does not rotate while the air above the equator rotates with the earth, and at the same velocity. Between the equator and the poles, points on the earth's surface and in the atmosphere above these points rotate at intermediate speeds, between zero and 28 km=min. When air moves between latitudes in which the speed of rotation is different, it is subject to the Coriolis effect, which gives the wind speed an unexpected component with respect to an observer on earth. For example, when a

32

2.6 GENERAL CIRCULATION OF THE ATMOSPHERE

parcel of air moves from one of the poles toward the equator, it is moving from an area where little or no rotation is taking place to an area where the earth is rotating quickly beneath it. This parcel of air tends to lag behind the rotating earth, that is, the earth is rotating away from this parcel of air, moving faster than the parcel of air from west to east. From the perspective of an observer who is rotating with the earth, this parcel of air seems to be moving backward (i.e., from east to west). In the Northern Hemisphere, where the parcel of cold air near the surface of the earth is moving north to south because of unequal heating, the overall result is to give this parcel of air a northeast-to-southwest motion with respect to someone on the earth's surface. We should therefore expect surface winds in the Northern Hemisphere to blow generally from the northeast. Similar reasoning would lead us to expect surface winds in the Southern Hemisphere to blow from the southeast. A simpli®ed version of the actual prevailing wind patterns on the earth's surface is shown in Figure 2-6. These prevailing surface wind patterns are most noticeable over the oceans and were of great practical importance in the days of large sailing ships, when the major wind systems received their names. The doldrums near the equator and the horse latitudes were much feared by sailors, because a ship could remain becalmed there for weeks at a time. The various wind belts have a tendency to shift north and south at times, and the winds sometimes reverse because of topographical features, weather patterns, or simply the greater variability of some of these wind systems. The trade winds and the prevailing westerlies are fairly reliable, at least over the larger oceans, but the polar easterlies barely exist. The prevailing westerlies in both

N 60⬚N

Polar easterlies Prevailing westerlies

30⬚N

Horse latitudes Northeast trade winds Doldrums

Equator

Southeast trade winds Horse latitudes

30⬚S

Prevailing westerlies 60⬚S S

Polar easterlies

FIGURE 2-6 An extremely simpli®ed version of prevailing wind patterns on the earth's surface. Polar easterlies, especially, are relatively insigni®cant.

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

33

hemispheres seem to be blowing in the wrong direction, at least according to Hadley's original ideas, moving from the southwest instead of the northeast in the Northern Hemisphere and from the northwest instead of the southeast in the Southern Hemisphere. Air is therefore ¯owing from the equator to the poles along the surface of the earth in these midlatitude regions, and is moving from a more rapidly rotating region of the earth's surface to a more slowly rotating region. Thus, these portions of the atmosphere are moving west to east faster than their destination, and the winds, which are a manifestation of this moving air, have a westerly component. In summary, therefore, near the equator and near the poles, cold air is moving toward the equator near the surface of the earth with an apparent easterly (east-to-west) component, while, in the midlatitudes, warm air is moving from the equator toward the poles along the surface of the earth with a westerly (west-to-east) component. As stated earlier, these easterly and westerly components of winds moving between portions of the earth that rotate at different speeds are manifestations of the Coriolis effect. The three main prevailing wind directions in each hemisphere have been explained in terms of a three-cell model (Figure 2-7) as distinguished from Hadley's original one-cell model (Figure 2-5). The current model has warm air rising at the equator and sinking near the poles just like the original Hadley model. The air circulation systems closest to the equator and to the poles move in the expected directions, with cold air traveling toward the equator near the surface of the earth, resulting in easterly winds. At latitudes 308N and 308S, these cells have downward moving air, while at 608N and 608S, they have upward moving air. To preserve these wind directions, the midlatitude cells have warm air moving from the equator toward the poles near the earth's surface, resulting in westerlies. The three-cell model, designed by Rossby in

N

60⬚N

30⬚N

Equator

FIGURE 2-7 Three-cell model of general atmospheric circulation in the Northern Hemisphere.

34

2.6 GENERAL CIRCULATION OF THE ATMOSPHERE

1941, is also quite oversimpli®ed because it gives the appearance that the cells are ®xed in place and that there is almost no air circulation between cells. In fact, the boundaries of the cells move, and the mixing of parcels of air coming from different parts of the globe varies quite a bit with the seasons (see Section 5.2.3.3). Nevertheless, the three-cell model is a great improvement over the one-cell model because any model that has only easterly winds all over the globe is impossible. Such unidirectional winds would tend to slow down the earth's west-to-east rotation. In fact, easterly and westerly winds must balance on the average, since the atmosphere as a whole rotates with the earth. This fact was ignored in the single-cell model. The simple scheme shown in Figures 2-6 and 2-7, although it explains the major prevailing wind systems on the earth's surface reasonably well, cannot adequately explain numerous other atmospheric phenomena. These include the so-called jet stream in the upper troposphere, which ¯ows west to east, the systems of low and high pressure with circulating winds that constitute our weather systems, and the general west-to-east movement of these weather systems. It turns out that a good deal of energy is transmitted from the equatorial regions to the polar regions by these so-called cyclone and anticyclone weather systems. Further explanations are outside the scope of this chapter. Let us just note here the results of experiments with model liquid systems (i.e., suspensions of metal powders in liquids under conditions that simulate conditions in the earth's atmosphere) have shown, under certain conditions, ¯ow patterns that correspond to the type of air circulation in cyclones and anticyclones and the slow drift of these ¯ow patterns in the direction of motion of the fastest moving portion of liquid. The circulation experiments are carried out as follows. A liquid suspension is placed between two cylinders; the inner cylinder is cooled and stationary, while the outer cylinder is heated and rotating. The metal particles in the suspension can be seen in motion back and forth between the stationary cold cylinder wall and the rotating warm cylinder wall. Eddies sometimes form, and these can be seen moving in the direction of rotation of the outer cylinder, but much more slowly. Figure 2-8, taken from a report of one of these experiments, permits us to visualize the patterns that are observed. Both the steady waves and the irregular patterns in Figure 2-8 look somewhat like diagrams of the upper atmosphere jet stream seen with the North Pole at the center. The jet stream, observed in this way, has lobes going alternately north and south in which air travels generally west to east, in the direction of earth's rotation. The jet stream moves in the middle latitudes of the hemisphere. In the continental United States, which is in the northern midlatitude zone, everything contributes toward a general west-to-east movement of the atmosphere. This is the region of prevailing westerlies, the jet stream moves west to east, and all major weather systems move west to east. This is why so many sulfur and nitrogen compounds from industrially polluted air seem to end up in

35

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

(I) symmetric (Ω = 0.341 rad s–1)

(II) steady waves (Ω = 1.19 rad s–1)

(III) irregular (Ω = 5.02 rad s–1)

FIGURE 2-8 Drawings made from photographs illustrating three typical top-surface ¯ow patterns of free thermal convection in a wall-heated rotating ¯uid annulus; inner wall at 16.38C; outer wall at 25.88C; working ¯uid, water. From R. Hide, ``Some laboratory experiments on free thermal convection in a rotating ¯uid subject to a horizontal temperature gradient and their relation to the theory of global atmospheric circulation,'' In The Global Circulation of the Atmosphere (G. A. Corby, ed.). Royal Meteorological Society, London. Copyright # 1969. Used by permission of the Royal Meteorological Society.

rainfall over New England (northeastern sector), as mentioned earlier. Both the jet stream (in the upper troposphere) and our general weather systems contribute to the west±east motion of polluted air over the continental United States. There is also some north±south and south±north movement of polluted air at different times, especially between our industrial Midwest and south-central Canada. Furthermore, in Europe, polluted air seems to move generally southwest to northeast, causing problems for the Scandinavian countries which are thus in the path of pollutants transported from the United Kingdom and from central Europe. At one time, people believed that virtually all the heat transfer from the equator to the poles occurred via the earth's atmosphere. It is now surmised that ocean currents like the Gulf stream perform about 50% of all heat transport between the equator and the poles; only half the heat is transported by the atmosphere.

2.7 CONCLUSION In this chapter, we have examined the constituents of the earth's atmosphere and brie¯y discussed their origins. We have learned about the general temperature and pressure pro®le of the atmosphere and how and why, in general, it circulates around the earth. Up to this point, then, we have enough

36

EXERCISES

information to think about the answers to question 4 in Section 2.1. Winds, including the jet stream, occur mostly in the troposphere, but there must also be circulation patterns in the stratosphere to help distribute the ozone, which is produced mostly in the stratosphere above the tropics, to the regions above the poles.

""!/!*$&( Reading (see also Chapter 3) Calder, N., The Weather Machine. How Our Weather Works and Why It Is Changing. Viking, New York, 1974. Deepak, A., ed., Atmospheric Aerosols. Their Formation, Optical Properties, and Effects. Spectrum Press, Hampton, VA, 1982. The Enigma of Weather. A Collection of Works Exploring the Dynamics of Meteorological Phenomena. Scienti®c American, New York, 1994. Finlayson-Pitts, B. J. and Pitts, J. N. Jr., Chemistry of the Upper and Lower Atmosphere: Theory, Experiments, and Applications. Academic Press, New York, 2000. Inadvertent Climate Modi®cation. A Report on the Study of Man's Impact on Climate (SMIC). MIT Press, Cambridge, MA, 1971. Macalady, D. L., ed., Perspectives in Environmental Chemistry. Oxford University Press, New York, 1998. Schneider, S. H., and R. Londer, The Coevolution of Climate and Life. Sierra Club Books, San Francisco, 1984. Siskind, D. E., S. D. Eckerman, and M. E. Summers, eds., Atmospheric Science Across the Stratopause, American Geophysical Union, Washington, DC, 2000. U.S. Standard Atmosphere, 1962; and U.S. Standard Atmosphere Supplements, 1966. U.S. Government Printing Of®ce, Washington, DC. Wayne, R. P., Chemistry of Atmospheres, 2nd ed. Clarendon Press, Oxford, 1991. Walker, J. C. G., Evolution of the Atmosphere. Macmillan, New York, 1977.

EXERCISES 2.1. It is well known that the minimum altitude of the ionosphere is higher at night than during the day. Why might this be true? 2.2. Explain why the temperature of the earth's atmosphere increases (a) from about 15 to 50 km above the earth's surface, and (b) from about 85 km to the outer limits of the earth's atmosphere. 2.3. What are the three major in¯uences that control earth's atmospheric circulation? Explain the effect of each of these. 2.4. The South Pole, during its midsummer, receives more solar energy during 24 h than any other place on earth, yet it remains extremely cold. Why might this be true? 2.5. A few air pollution experts have accumulated a small amount of evidence indicating that some of the smog particles from Los Angeles eventually come to earth in the vicinity of Albany, New York.

2. ATMOSPHERIC COMPOSITION AND BEHAVIOR

37

(a) Is this possible? Why or why not? (b) Is this probable? Why or why not? 2.6. What compounds in the earth's atmosphere are considered to be responsible for acid rain? Why is rain with pH 5.5 not considered to be acid rain? 2.7. Make a sketch of the temperature pro®le of the earth's atmosphere without looking at Figure 2-4. The ordinate is altitude and the abscissa is temperature. Label the main parts of the atmosphere. Put in approximate temperatures in appropriate places. 2.8. There are several portions of the atmosphere in which the temperature change with altitude indicates that chemical reactions must be taking place. Name each of these parts of the atmosphere, and brie¯y describe the types of reaction taking place. Indicate why the reactions are different in different portions of the atmosphere.

3 ENERGY AND CLIMATE

3.1 ENERGY BALANCE OF THE EARTH 3.1.1 Incoming Radiation from the Sun The discussion on the general circulation of the atmosphere in Chapter 2 presupposed that most of the heating of the earth's surface comes from solar radiation. The total
solar energy reaching the surface of the earth each year is  about 2
1021 kJ 5
1020 kcal . Heat generated by radioactive
processes in the earth and conduction from the core contribute 8

1017 kJ  2
1017 kcal, and human activities contribute about 4
1017 kJ 1017 kcal per year. This means that less than 0.1% of the total energy reaching the earth's surface each year comes from processes other than direct solar radiation. For the purposes of this chapter, therefore, we may treat the energy input to the earth as if it all came from the sun. The sun is almost a blackbody radiator (with superimposed line spectra); a perfect blackbody is one that absorbs all radiation impinging on it; it also emits the maximum possible energy at any given temperature. The energy emitted 39

40

3.1 ENERGY BALANCE OF THE EARTH

from unit area of the blackbody per unit wavelength per unit solid angle in unit time, Bl (T), is given by Planck's blackbody equation: Bl T dl 

2hc2 dl l5 exphc=lkT   1

3-1

where k  1:38
1023 J molecule1 K1 is Boltzmann's constant (the gas constant per molecule), h is Planck's constant, 6:63
1034 Js, c is the speed of light in vacuum, 3:00
108 m/s, l is the wavelength of interest in meters, and T is the absolute temperature in kelvin. Since the sun is emitting radiation mostly from its surface, and since we shall also wish to consider blackbody radiation from the surface of the earth, we shall rewrite equation (3-1) in the form Il 

C1 l expC2 =lT   1

3-2

5

where Il is the radiation intensity emitted by each square meter of surface of the blackbody at wavelength l, T is the absolute temperature, C1  3:74
1016 Wm2 , and C2  1:438
102 mK (the symbol W refers to watts). The total intensity of radiation emitted by a blackbody at any temperature is given by the Stefan±Boltzmann law, I  sT 4 4

3-3 1

4

where s  5:672
108 W m2 K  8:22
1011 cal cm2 min K . The relative distribution of energy, proportional to equation (3-2), is plotted in Figure 3-1 as a function of wavelength for two temperatures. One may see that there is a wavelength of maximum emission lmax that shifts to lower wavelengths as the temperature is increased. Most commonly, the wavelength of maximum blackbody emission is encountered in the infrared (e.g, the 3300 K curve in Figure 3-1 corresponds approximately to the output of a 200-W tungsten ®lament lamp). However, at 6000 K (roughly the blackbody temperature of the sun), lmax is in the visible region (480 nm). Ninety percent of the solar radiation is in the visible and infrared, from 0.4 to 4.0 mm, with almost constant intensity (but see Section 3.3.1). The other 10% of the solar radiation intensity varies somewhat with time in the ultraviolet region and becomes extremely variable in the x-ray region of the spectrum. The wavelength at which maximum emission of radiation occurs at any temperature is given by Wien's displacement law, lm T  2897:8 mmK

3-4

Solar radiation is emitted in all directions from the sun, and very little of this reaches earth. In fact, earth is so far away from the sun that it picks up only about 2
109 of the total solar energy output. At a distance from the sun

41

3. ENERGY AND CLIMATE

Ultraviolet

Visible

Infrared

1.0

Relative intensity

0.8

0.6

B 0.4

0.2 A

200

400

600 800 1000 Wavelength (nm)

1200

FIGURE 3-1 Distribution of energy from a blackbody radiator at 3300 K (curve A) and 6000 K (curve B).

equal to the average radius of the earth's orbit, the solar energy passing any surface perpendicular to the solar radiation beam is 1367 4 kW=m2
1:95 cal cm2 min1 ; this is called the solar constant for the earth. Since the earth does not consist of a plane surface perpendicular to the path of the solar radiation but presents a hemispherical surface toward the sun, a recalculation of the solar constant must be made for radiation falling on this hemispherical surface. Actually, since we wish to use an average radiation intensity averaged over the total surface of the earth, we must compare the surface area of the whole earth, 4pr2 , where r is the radius of the earth, with the area that the earth projects perpendicular to the sun's rays, pr2 (see Figure 3-2). Thus, the earth's surface has four times the area of the circle it projects on a plane perpendicular to the sun's rays, if these rays are assumed parallel at such large distances from the sun. Therefore, the solar radiation that comes in toward the earth's surface is one-fourth of the solar constant, or approximately 343 W=m2, averaged over the whole surface. These numbers indicate

42

3.1 ENERGY BALANCE OF THE EARTH

Earth’s surface area = 4πr 2

Projection of Earth on perpendicular plane has area = πr 2 Plane perpendicular to sun’s rays

Solar radiation, assuming parallel rays

FIGURE 3-2 Comparison of earth's surface area with the area of earth's projection on a plane perpendicular to the sun's rays.

the total amount of solar radiation coming in to the top of the earth's atmosphere; some of this radiation is absorbed in the atmosphere and some is re¯ected. The solar radiation that actually penetrates to the surface of the earth below the atmosphere no longer has the spectral distribution of black body radiation from a body at 6000 K (Figure 3-1). Figure 3-3 shows that no solar radiation with wavelength below 0.28 mm (280 nm) reaches the surface of the earth. We already knew this, from the discussion of absorption by oxygen in the thermosphere and by ozone and oxygen in the stratosphere (Section 2.5). The absorption of solar infrared radiation has not been discussed yet, but a large portion of the sun's infrared radiation is absorbed by water vapor, carbon dioxide, and trace gases in the atmosphere. Figure 3-4 speci®cally shows the absorption of solar radiation by water and carbon dioxide in the atmosphere; one can see that this absorption is complete at some wavelengths. The absorption of solar infrared radiation by various constituents of the atmosphere is not very important because comparatively little of the solar radiation is in the infrared (Figures 3-1 and 3-3). These absorptions become much more important when we consider radiation emitted by the earth. It should be fairly obvious that the earth is emitting radiation because, on the average, the earth is in thermal equilibrium. It is in the path of 2
1021 kJ of solar radiation each year, and it is necessary that 2
1021 kJ per year leave the earth. If less energy than that leaves the earth, it will become hotter. Some of the solar energy, as we shall see, is immediately re¯ected, but some is absorbed and must be reemitted.

43

3. ENERGY AND CLIMATE

Ultraviolet

Atmospheric transmission

Frequency (Hz)1016 1.0

10

V i s i b l e 15

Infrared

1014

Sub-mm

1013

Microwave

1011

1012

1010

0.5

109

Radar bands K X C S L

0 0.0 µm

0.1 µm

1.0 µm

10 µm 100 µm 0.1 cm Wavelength,

1.0 cm

10 cm

P

100 cm

FIGURE 3-3 The transmission spectrum of the upper atmosphere: low transmission means high absorption. Redrawn from J. E. Harries, Earthwatch, The Climate from Space. Horwood, New York, Copyright # 1990.

25

(102 Wm–2 µm–1)

20

15

O3 H2O O2, H2O

10

H2O H2O H2O H2O H2O, CO2

5

H2O, CO2 H2O, CO2

O3 0

0

0.5

1.0

1.5 (µm)

2.0

2.5

3.0

FIGURE 3-4 Spectral distribution of solar irradiation at the top of the atmosphere and at sea level for average atmospheric conditions for the sun at zenith. Shaded areas represent absorption by various atmospheric gases. Unshaded area between the two curves represents the portion of the solar energy backscattered by the air,
 vapor, dust, and aerosols and re¯ected by clouds. Redrawn from J. P. Peinuto and A. H. Oort, Physics of Climate. American Institute of Physics, New York. Copyright # 1992 by Springer-Verlag GmbH & Co. Used by permission of the publisher.

44

3.1 ENERGY BALANCE OF THE EARTH

3.1.2 The Greenhouse Effect The present average temperature T of the earth's surface, taken at any one time over the whole surface of the earth, is close to 158C (288 K). Thus, even though the temperature varies with time and place, the earth's surface must therefore radiate much like a blackbody at 158C. Figure 3-5 shows the intensity of emission Il for blackbodies at 255 and 288 K. The wavelength for maximum radiation intensity is about 10 mm in this temperature range, that is, in the infrared region of the spectrum. We should be able to ®nd the average value of the earth's radiation temperature by calculationÐby balancing incoming and outgoing radiation at the earth's surface. We shall call this mean radiation temperature Tr . Let us assume that energy in  energy out, ignoring radioactivity and human activities. We know from satellite measurements that the earth re¯ects about 30% of the total incoming solar radiation, so that only 70% is absorbed. Therefore, Iin  Iout  070
343 W=m2 . Using the Stefan±Boltzmann law, equation (3-3), we have

7 288 K 255 K

6

I( ) (arbitrary units)

5

4

3

2

1

0 0

10

20 30 Wavelength ( m)

40

50

FIGURE 3-5 Radiation intensity (in arbitrary units) versus wavelength for black bodies at 255 K (dashed curve) and 288 K (solid curve).

45

3. ENERGY AND CLIMATE

07
343 W=m2 Tr  5:67
108 W m2 K4 

1=4

 255 K  188C

3-5

Therefore, to satisfy the law of conservation of energy, the earth±atmosphere system must be radiating energy into space at an average of 188C. Therefore, the earth cannot be radiating energy out into space directly from its surface, at least on the average. Average temperatures in the neighborhood of 188C are found in only two places from which radiation could logically occur: near the tropopause and in the region of the mesopause in the upper atmosphere. Since radiation cannot occur in the atmosphere unless many molecules are present to radiate, it is probable that most of the earth's radiation into space occurs from the atmosphere near the tropopause, probably the upper regions of the troposphere. This leaves us with two related questions: Why does the earth radiate to space mostly from the atmosphere and not from the surface, and why is the surface of the earth hotter than it should be, considering the energy balance calculations? That is, what traps heat between the surface of the earth and the tropopause? Both these questions have to do with the absorption of infrared radiation by atmospheric water vapor, carbon dioxide, methane, and small amounts of other gases. Figure 3-5 shows that the earth's radiation is almost all in the infrared, whether we consider radiation from the surface (blackbody at 158C  288 K) or from the atmosphere (blackbody at 188C  255 K). The absorption bands from 1.0 to 15:0 mm of CO, CH4 , H2 O, CO2 , and some of the other gases present in the earth's atmosphere are shown in Figure 3-6. The fraction of the earth's radiation absorbed at each wavelength depends on the amount of each gas present in the atmosphere and on the ``strength'' of each absorption band. Looking at Figure 3-6, one may observe that the gases normally in the atmosphere absorb in different regions of the infrared. In fact, the earth's infrared radiation is absorbed almost completely in many wavelength regions; this is true except in those wavelength regions that are called ``atmospheric windows.'' These can be seen in Figures 3-3 and 3-6 as the regions in which the atmospheric transmission is close to 1.0 (Figure 3-3) or 100% (Figure 3-6). As we expect, Figure 3-3 shows that the atmosphere is almost completely transparent in the visible region of the spectrum, and that there are numerous complete and partial ``windows'' in the infrared. Both ®gures show that the region above 14 mm is almost completely opaque to infrared radiation, but the atmosphere is mostly transparent to the longer wavelength microwave radiation, especially the region that Figure 3-3 shows as radar bands. Water vapor, which has more absorption bands than any of the other gases at almost all wavelengths shown in Figure 3-6, is the most important absorber of infrared radiation in the earth's atmosphere. After water vapor, CO2 and O3 are second and third in importance, respectively. The main atmospheric ``window'' (see Figures 3-5 and 3-6) is between about 8 and 12 mm except for a region

46

3.1 ENERGY BALANCE OF THE EARTH

0

100 CO

CH4

100 0

N 2O

100 0

CO2

100 0

H2O

100 0

0 100 0 100

O3

100 0

0 100

Collective absorption

100

0 100 0 100

Transmission (percent)

Absorption (percent)

100 0

0 100

0 2

4

6

8 10 Wavelength (µm)

12

14

16

FIGURE 3-6 Absorption of some atmospheric gases in the infrared spectral region. Redrawn from M. L. Salby, Fundamentals of Atmospheric Physics. Copyright # 1996. Used by permission of Academic Press.

around 95 mm, in which O3 is a strong absorber. We may note from Figure 3-6 that there are absorption bands of CO2 in the atmospheric ``windows'' just below 5 mm and near 10 and 13 mm. CH4 absorbs in the atmospheric ``window'' near 8 mm. This means that changes in the atmospheric concentration of these gases, and of others, including the chloro¯uorocarbons discussed in Section 5.2.3.2, which can absorb more radiation in the infrared ``windows,'' will be important in the discussion of global climate changes in Section 3.3.3. When the sky is clear, terrestrial radiation in the wavelength region of the ``windows'' escapes directly to space. Clouds, when present, re¯ect this radiation back to the earth's surface and the radiation does not escape. However, on clear nights, especially in the winter, we have the phenomenon of ``radiation cooling'' of the earth's surface through the atmospheric ``windows.''

3. ENERGY AND CLIMATE

47

The infrared radiation that is absorbed in the troposphere and in the stratosphere would warm these regions of the atmosphere substantially if energy were not also radiated from these regions. This is the energy radiated at an average temperature of 188C (this average includes the higher temperatures at which radiation from the earth's surface escapes through the atmospheric windows) that leaves the earth. Thus, the atmosphere intercepts infrared radiation from the earth's surface and then reradiates the energy both back toward the earth's surface, thus warming it, and upward to space, thus cooling the earth so that the constant solar radiation does not slowly increase the earth's temperature. The earth's surface can therefore be much warmer than the average radiation temperature of the earth. This phenomenon is usually called the ``greenhouse effect'' because a related phenomenon is observed in a closed greenhouse. The glass or plastic windows of the greenhouse allow the visible solar radiation to enter the inside, but the upward-directed infrared radiation from the ¯oor is absorbed or re¯ected by the same windows. In contrast to the ``greenhouse effect'' in the atmosphere, however, energy retention in the greenhouse is caused mostly by lack of convection (i.e., lack of mixing of the interior air with the surrounding atmosphere). The same effect occurs in a closed automobile that is left out in the sun. Both the greenhouse and the car interiors may thus become considerably warmer than the temperature of the surrounding atmosphere. A greenhouse coef®cient may be de®ned as the ratio of the surface temperature to the absolute radiation temperature of the whole system. For the earth, this coef®cient is 288 K=255 K  1:13, while for the planet Venus it appears to be 743 K=233 K  3:2! Venus thus has a much larger greenhouse effect than earth; this is presently believed to be caused by carbon dioxide, sulfur dioxide, and possibly chlorine gas in the Venusian atmosphere. The Martian atmosphere contains mostly carbon dioxide but is so thin that the greenhouse coef®cient is only 218 K=212 K  1:03. For quantitative discussions of the greenhouse effect on earth, it is convenient to de®ne the greenhouse effect somewhat differently, as discussed and calculated in Section 3.3.1. Further discussions of the greenhouse effect on earth, and how this effect may vary with changes in the content of carbon dioxide and other trace gases in the atmosphere, are in Section 3.3.3.

3.1.3 Other Factors The mean temperature of the earth's surface is certainly affected by the magnitude of the greenhouse effect, but it is also affected by the percentage of incoming solar radiation that is re¯ected back out to space, that is, by the earth's albedo. It has already been stated that approximately 30% of the incoming radiation is immediately re¯ected. This is an average value;

48

3.1 ENERGY BALANCE OF THE EARTH

Table 3-1 shows the albedo of various major features on earth. Major changes in cloud cover, snow and ice, ®eld and forest, and so on would change the average albedo of the earth. For example, a decrease in snow and ice cover would decrease the earth's albedo, thus leading to absorption of more solar radiation and, in the absence of other effects, a higher surface temperature for the earth. As it turns out, however, clouds also contribute to the greenhouse effectÐthey re¯ect some of the earth's infrared radiation back to earth instead of reradiating it like the atmospheric greenhouse gases. In the simplest picture, however, like the one considered in this book, clouds are considered only with respect to their re¯ectivity. These and other factors in the energy balance of the earth are also important as shown schematically in Figure 3-7. The left-hand side of Figure 3-7 shows that 30% of the 343 W=m2 that comes toward the earth from the sun is immediately re¯ected with no change, that water vapor and clouds in the troposphere and ozone and other ultraviolet absorbers remove an additional 20% of the total, and that the remaining 50% of the incoming radiation, about 172 W=m2 , is absorbed by the earth's surface. The central portion of Figure 3-7 shows the fate of the radiation from the earth's surface (at 158C), about 390 W=m2 , which is 114% of the solar energy that enters the atmosphere (a result of the greenhouse effect, Section 3.1.2). Most of this energy is absorbed and reemitted (or re¯ected) by clouds and gases in the atmosphere. Other types of energy transfer also occur, as shown on the right-hand side of Figure 3-7. Latent heat transport refers to the heat of vaporization of water; water evaporates from the surface of the earth, thus cooling the surface, and then condenses in the atmosphere, thus heating the atmosphere. Sensible heat transfer refers to heat transfer by convection as heated air near the ground rises while cooler air higher in the troposphere sinks. TABLE 3-1 Albedo of Various Atmospheric and Surface Features of the Earth Albedo (% re¯ected) 30 50±80 40±95 16±20 20±25 15±25 5±20 18±28 14±18 7±20 7±23

Re¯ected from Total (earth and atmosphere) Clouds Snow and ice Grass Dry, plowed ®elds Green crops Forests Sand Cities Bare ground Oceans

49

3. ENERGY AND CLIMATE

30

10

60

100 Space Atmosphere

Absorbed 20

Absorbed 100

Emitted 150

Sensible 5

Latent 25

110 90 Surface Absorbed solar 50

Net terrestrial radiation −20 (emitted)

Net terrestrial nonradiative −30 (emitted)

Solar

Terrestrial

Nonradiative

FIGURE 3-7 Energy±¯ux diagram showing radiative and nonradiative exchanges between the earth's surface, the atmosphere, and space. Units are percentages of global-average insolation (100%  343 W=m). The ¯ux at the surface exceeds 100% of the solar energy ¯ux reaching the earth because of the absorption±emission cycle between the surface and the atmosphere. Redrawn from G. J. MacDonald and L. Sertorio, eds., Global Climate and Ecosystem Change. Plenum Press, New York. Copyright # 1990. Used by permission of Kluwer Academic=Plenum Publishers.

3.2 CLIMATE HISTORY OF THE EARTH Before trying to decide whether humans are actually succeeding in changing the earth's climate at present, we must consider what sorts of climate change occurred before humans evolved, and what climate changes occurred before the major industrialization of the twentieth century. It is, unfortunately, beyond the scope of this chapter to discuss the various methods of calculating average temperatures at different times in the past; these methods are discussed in some of the references at the end of the chapter. The variation of the mean surface temperature of the earth between the latitudes 408N and 908N as a nonlinear function of time from 500,000,000 b.c. to a.d. 1950 is shown in Figure 3-8. The time scale is arranged to emphasize recent years, for which more reliable data are available. More recent times are shown in more detail in Figure 3-9. Glacial periods occurred at intervals between 10,000 and 1,000,000 b.c. It looks, from Figure 3-8, as though there have also been major glacial episodes around 200,000,000 b.c.

50

3.2 CLIMATE HISTORY OF THE EARTH

T(⬚C)

10 5

B.C.

2,000

1,500

5,000 1,000 500 0 500 1,000

50,000 10,000

100,000

500,000

1,000,000

50,000,000

100,000,000

−5

500,000,000

0

A.D.

FIGURE 3-8 Temperature variations in the Northern Hemisphere (408N ± 908N) as a function of time. Redrawn, by permission of the publisher, from J. E. Oliver, Climate and Man's Environment. Copyright # 1973, John Wiley & Sons, Inc.

and 500,000,000 b.c. In general, the average temperatures before 1,000,000 b.c. were warmer than those that have occurred since that time. Since 1,000,000 b.c., the interglacial periods, although warmer than either the glacial periods or the present, were much cooler than the eras before that time. Notice that the difference in average temperatures between glacial and interglacial periods was only about 58C; that is, comparatively small differences in average temperature have large effects on the total climate. Notice also that variations up to 28C have occurred since a.d. 1000. This means that average temperatures in the Northern Hemisphere have varied appreciably before human activities could have had any effect. Figures 3-8 and 3-9 deal with very long-term variations in average temperature. If we are interested in climate changes possibly attributable to human intervention, we shall have to focus on much shorter term ¯uctuations. Let us, however, start with the period from 4000 to 3000 b.c. (6000±5000 years before the present), where Figures 3-8 and 3-9 show a temperature maximum, the ``Holocene maximum.'' During this time many glaciers had melted, and sea level was much higher than it is today, and major civilizations existed in Egypt. Between 3000 and 750 b.c. the world generally become somewhat cooler, glaciers advanced, and sea level dropped. Canals were constructed in Egypt to take care of problems associated with the general drop in water levels. Another warming trend culminated in about a.d. 1200, the ``medieval warm period,'' the warmest climate in several thousand years in the Northern Hemisphere. Glaciers retreated so far that the Vikings were able to travel to and settle in Greenland and Iceland. Southern Greenland had average temperatures 2±48C above present temperatures while Europe had about 18C higher average temperatures than at present.

51

Temperature change (⬚C)

3. ENERGY AND CLIMATE

(a)

Previous ice ages

Temperature change (⬚C)

800,000

600,000 400,000 Years before present

200,000

Holocene maximum

(b)

10,000

Temperature change (⬚C)

Last ice age

8,000 6,000 4,000 Years before present

Little ice age

2,000

0

(c) Little ice age

Medieval warm period

1000 A.D.

1500 A.D. Year

1900 A.D.

FIGURE 3-9 Schematic diagrams of global temperature variations since the Pleistocene on three time scales: (a) the last million years, (b) the last ten thousand years, and (c) the last thousand years. Dotted line nominally represents conditions near the beginning of the twentieth century. Redrawn from J. T. Houghton, G. J. Jenkins, and J. J. Ephraums, eds., Climate Change. The IPCC Scienti®c Assessment. Cambridge University Press, New York. Copyright # 1990. Used by permission of the Intergovernmental Panel on Climate Change.

52

3.2 CLIMATE HISTORY OF THE EARTH

Between a.d. 1300 and 1450, there was a cooling trend that made it harder for ships to travel between Greenland and Iceland and made Greenland cool enough to cause the Vikings to abandon their settlements. A warming trend between 1450 and 1500 was followed by the ``Little Ice Age,'' which did not end in some areas until 1850. Glaciers advanced and winters were very cold in this period. Since 1850, there has been a distinct warming trend, with precipitous retreats of glaciers that ended temporarily around 1940 (see Figures 2-1 and 3-10). Figures 2-1 and 3-10 are very similar, but they refer to somewhat different time intervals and the temperature averages were obtained from somewhat different sources. Both ®gures show that the warming trend resumed about 1975. The retreat of the glaciers is easy enough to document, but these very short-term recent temperature trends are very hard to evaluate. First of all, while glaciers are retreating in one part of the world, they often are advancing elsewhere. What is the average trend? Furthermore, climate and temperatures are variable in any one place from year to year, and it is not easy to ®nd a general trend among ¯uctuations. The problem in the evaluation of short-term trends lies in variability in climate that occurs both from place to place and from year to year. The place-to-place variability can be taken care of by averaging temperatures over a large enough area; that is why we see a global mean land temperature in Figure 2-1 and a combined land and sea surface temperature in Figure 3-10. The year-to-year variability can be seen very clearly in both ®gures. The averages, however, still do not tell the whole story; in this period, they represent mostly an increase in the number of warm months during each year, not an overall increase in actual temperature. Furthermore, although the overall temperature changes have been similar in the

Temperature change (⬚C)

0.4 0.2 0.0 −0.2 −0.4 −0.6 1870

1890

1910

1930 Year

1950

1970

1990

FIGURE 3-10 Global±mean combined land±air and sea±surface temperatures, 1861±1989, relative to the average for 1951±1980. Redrawn from J. JaÈger and H. L. Ferguson, eds., Climate Change: Science, Impacts and Policy. Cambridge University Press, New York. Copyright # 1991. Used by permission of the Intergovernmental Panel on Climate Change.

3. ENERGY AND CLIMATE

53

Northern and Southern Hemispheres, the magnitudes have not been the same, and the warming and cooling trends did not necessarily occur in the same year, or, in some cases, in the same decade. Note that the variations shown in Figure 3-10 are generally less than 18C, but, as we have seen, it takes only about 58C to change from a glacial to an interglacial period. The greatest variability in average temperature appears generally to be near the poles, not near the equator. 3.3 CAUSES OF GLOBAL CLIMATE CHANGES 3.3.1 General Comments Climate is mainly effected by wind patterns over the earth's surface, and these changes in wind patterns are generally caused by changes in the earth's energy balance, as mediated, among other things, by changes in ocean currents and ocean temperatures. A well-known example is the El NinÄo=Southern Oscillation (ENSO), the eastward (toward South America) expansion of a pool of warm water usually found in the western Paci®c Ocean; global temperatures generally rise during an ENSO. The average surface temperature of the earth can be calculated in principle by employing the concepts discussed in Section 3.1. The starting point, as in Section 3.1, is Iin  Iout , where Iin  S=41  a and Iout  I0  DI. In these expressions S is the solar constant, a is the earth's albedo, I0 is the intensity of radiation emitted at the earth's surface, I0  sT 4 , T is the mean surface temperature of the earth; and DI is a term involving the greenhouse effect. Substituting for I0 and solving for T, we have   S1  a=4 DI 1=4 T 3-6 s The variables in equation (3-6), S, a, and DI, are called ``climate forcing agents'' because changes in these variables ``force'' changes in climate. If we take T, the average surface temperature of the earth, as an indicator of climate, then equation (3-6) allows us to determine the main factors that affect climate and even the magnitudes of possible effects. It can be seen that the solar constant, the earth's albedo, and the greenhouse effect all help to determine T. It has always been tempting to attribute major climatic variations, like those between glacial and interglacial periods, to variations in the solar constant, that is, to variations in solar irradiation. There is considerable evidence for this hypothesis, more because of variations in the earth's orbit and in the inclination of different latitudes toward the sun during different seasons (see Section 3.3.2) than because of major changes in the emission of radiation from the sun. The sun is quite variable in its emission of x-rays and even some ultraviolet

54

3.3 CAUSES OF GLOBAL CLIMATE CHANGES

radiation, but the emission of visible and infrared radiation seems to be quite steady, increasing, however, about 0.12% from the minimum to the maximum number of sunspots in the (usually) 11-year sunspot cycle (see Figure 3-11). Small climate changes have been associated with the sunspot cycle during this century, but 11 years is a short time and there are many other in¯uences on climate. Some extreme variations in sunspot activity have, however, been correlated with major peculiarities of climate. The coldest part of the ``little ice age'' appears to be concurrent with a 70-year minimum in sunspot activity during the late seventeenth and early eighteenth centuries, the ``Maunder minimum.'' There is some evidence that the solar constant decreased by about 0.14% during the Maunder minimum. We can use equation (3-6) to show that an 8% change in the solar constant could change the average surface temperature of the earth by 38C. The values of S, a, and s have been given in this chapter, and the present value of DI can be calculated from s, the measured mean surface temperature of the earth T, and the mean radiation temperature of the earth Tr as found in Section 3.1: DI  sT 4  Tr4  150 W=m2

3-7

The solar constant is presently being monitored by satellite measurements, and thus proper evaluations of its effect on climate will be possible in the future.

Total Irradiance (W/m2)

1368.0

1367.5

1367.0

1880

1900

1920 1940 Year

1960

1980

FIGURE 3-11 Reconstructed solar irradiance from 1874 to 1988. Redrawn from J. T. Houghton, G. J. Jenkins, and J. J. Ephraums, eds., Climate Change, Science, Impacts, and Policy. Cambridge University Press. New York. Copyright # 1990. Used by permission of the Intergovernmental Panel on Climate Change.

3. ENERGY AND CLIMATE

55

3.3.2 The Milankovitch Theory of Earth's Orbital Variations The Milankovitch theory attempts to account for the existence of Ice Ages at various intervals (see Figure 3-9). This theory makes use of the dependence of the insolation, the total solar radiation impinging on the earth in different latitudes, on a number of factors involving the earth's revolution around the sun. There is quite a bit of controversy about the particular latitudes at which such variations in insolation are most important, but most workers feel that changes in insolation at high latitudes, closer to the poles than 608N or 608S, are the most important. The ®rst orbital variation, which affects all latitudes in a similar fashion, involves the change in the earth's orbit from almost circular to somewhat elliptical and back, with a somewhat variable period of 90,000±100,000 years. When the earth's orbit is at its highest ellipticity, the solar radiation intensity reaching the earth may vary up to 30% in the course of a year. Right now, the earth's orbit is not very elliptical and indeed is becoming more circular. The second orbital in¯uence on solar irradiation, which affects different latitudes differently, is the 21,000-year cycle in the precession of the earth's axis around the normal to the earth's orbit; this changes the season at which the Northern (or Southern) Hemisphere is closer to the sun. This in¯uence is most important when the earth's orbit is even a little bit elliptical, as it is now. At present, for example, the earth is about 3
106 miles closer to the sun during winter in the Northern Hemisphere than during winter in the Southern Hemisphere. This means that there is about 7% less solar irradiation during summer in the Northern Hemisphere than during summer in the Southern Hemisphere.1 The third orbital in¯uence on solar irradiation at different latitudes is the 40,000-year cycle in the tilt of the earth's axis with respect to the normal to the plane of the earth's orbit. This angle varies between 21.8 and 24.4 degrees; at present, it is 23.4 degrees. These three types of orbital variation, with three different cycle lengths, have been used in various climate models to calculate average global temperatures in the absence of true solar constant variations and in the absence of changes in the greenhouse effect or earth's albedo for at least one million years before the present. Figure 3-12 is one of many comparisons between the calculations from the Milankovitch theory and actual measurements. (The ``measurements'' are actually reasonable guesses from various geological data.) The calculations were based on the assumption that the variation in insolation at latitude 508N could be used if one further assumed that whenever 1

This cycle is also connected with the change in the polestar, presently Polaris (almost); in 2600 b.c. the polestar was Alpha Draconis, about 25 celestial degrees away from Polaris.

56

Measured

3.3 CAUSES OF GLOBAL CLIMATE CHANGES

700,00 years ago

Present Warm Cold

Warm Cold Predicted

FIGURE 3-12 Comparison of warm and cold periods in the earth's climate as measured from geological data and as predicted from the Milankovitch theory. Redrawn from N. Calder, The Weather Machine. Viking Press, New York. London: BBC. Copyright # 1974. Used by permission of the author.

the summer sunshine at that latitude was at least 2% stronger than at present, glaciers tended to disappear, and that ice began to accumulate when the summer sunshine was less. Figure 3-12 shows reasonable agreement between the measured and calculated results. More complex assumptions have recently led to even better agreement between measured and calculated results. Therefore, we have a reasonable explanation for the existence of Ice Ages and interglacial periods. These orbital cycles exist and must interact with the other in¯uences on the earth's climate. 3.3.3 Greenhouse Effect Changes Small changes in the greenhouse effect DI can have appreciable effects on climate. These changes can occur when variations occur in the concentration of carbon dioxide, methane, and trace gases, especially those that can absorb radiation in the atmospheric ``windows'' as mentioned in Section 3.1.2. Figure 3-13 shows the close parallel between mean global temperature and the atmospheric carbon dioxide and methane concentrations as obtained from air trapped in Antarctic ice cores over the past 160,000 years. Although increased burning of fossil fuels is held responsible for the global increase in carbon dioxide concentration in the atmosphere during historic times, it appears that a major increase in carbon dioxide in the atmosphere started almost 20,000 years ago. Although this could be attributed to human activities, many of the other variations in carbon dioxide, and, for that matter, methane concentration, must have another cause. Figure 3-14 shows the recent (i.e., since 1840) increase in methane concentration in the atmosphere. In

57

3. ENERGY AND CLIMATE

2 0 −2 −4 −6 −8 −10

700 Methane

600 500 400

Carbon dioxide concentration (ppmv)

1990 Level of CO2 300 280 260 240 220 200 180

Carbon dioxide

0

Methane concentration (ppmv)

Local temperature change (⬚C)

preindustrial times, the atmospheric concentration of methane was about 0.8 ppm by volume, increasing to 1.75 ppm in 1999 and still increasing, although the rate of increase appears to have decreased during the past two decades. The recent changes in CO2 concentration in the atmosphere were shown in Figures 2-2 and 2-3. At any rate, there is de®nitely a positive correlation between the concentration of these gases and climate. Because of the known correlation between the concentrations of carbon dioxide and methane and climate, even though the actual connection is quite complicated, the concept of relative global warming potentials (GWPs) has been developed for all the so-called greenhouse gases, those that absorb infrared radiation in the ``atmospheric windows.'' This concept takes into account (1) the effect of an increase in concentration of the gas in the present

300 280 260 240 220 200 180

40 80 120 160 Age (thousand years before 1990)

FIGURE 3-13 Analysis of air trapped in Antarctic ice cores shows that methane and carbon dioxide concentrations were closely correlated with the local temperature over the last 160,000 years. The concentration of carbon dioxide is indicated on the left ordinate. Redrawn from J. Jager and H. L. Ferguson, eds., Climate Change: Science, Impacts and Policy. Cambridge University Press, New York. Copyright # 1991. Used by permission of the Intergovernmental Panel on Climate Change.

58

3.3 CAUSES OF GLOBAL CLIMATE CHANGES

CH4 concentration (ppb by volume)

1800

1600

1400

1200

1000

800

600 1820

1840

1860

1880

1900

1920

1940

1960

1980

2000

2020

Year FIGURE 3-14 Change in methane concentration in the earth's atmosphere since 1840.

atmosphere both in absolute terms and relative to carbon dioxide, (2) the effect of the different times that the various gases remain in the atmosphere, and (3) some of the reactions that these gases undergo in the atmosphere (see Chapter 5) over long periods. The results of factor 3 are called ``indirect effects'' and are not always included in the calculations of the GWP. At any rate, the GWP is thus the time-integrated warming effect expected from the instantaneous release of 1 kg of a given gas in today's atmosphere, relative to that expected from an equal mass of carbon dioxide. Table 3-2 shows the total GWPs, based on both direct and indirect effects, calculated over 20, 100, and 500 years for some gases with respect to the earth's atmospheric composition in 1990 along with the atmospheric lifetimes of these gases as used in the calculations. Carbon dioxide has the lowest GWP in the table, but its contribution to the greenhouse effect, and thus potential global warming, is very large because this contribution depends on the product of the GWP and the number of kilograms of the gas actually emitted. The CFC's in Table 3-2 are discussed at greater length in Section 5.2.3.2 because of their ability to destroy the ozone in the stratosphere. It is important, by the way, not to consider the greenhouse effect and the GWP in isolation from the other possible effects on climate, because both positive and negative feedback in¯uences are possible, as mentioned in Section 3.3.5.

59

3. ENERGY AND CLIMATE

TABLE 3-2 Atmospheric Lifetimes and Total Global Warming Potentials of Some Greenhouse Gases (Based on the Atmospheric Composition in 1990) Time horizon (years) Gas

Atmospheric lifetime (years) 20

CO2 CH4 N2 O CFC-11a CFC-12a HCFC-22a

10.5 132 55 116 16

1 63 270 4500 7100 4100

100

500

1 21 290 3500 7300 1500

1 9 190 1500 4500 510

a

CFC's are chloro¯uorocarbons while HCFC's are hydrochloro¯uorocarbons. The composition of each one can be determined by using the Rule of 90 as follows: add 90 to the number in the name of the gas. A number larger than 100 will be obtained, for example, 101 for CFC-11. The ®rst digit is the number of C atoms, the second is the number of H atoms, the third is the number of F atoms, and the number of Cl atoms is obtained by assuming that the molecule contains no double or triple bonds or rings. Thus, CFC-11 is CFCl3 , CFC-12 is CF2 Cl2 , and HCFC-22 is CHF2 Cl. Source: J. T. Houghton, G. J. Jenkins, and J. J. Ephraums, eds., Climate Change: The IPCC Scienti®c Assessment. Cambridge University Press, Cambridge, U.K., 1990.

Let us note that not all the carbon dioxide emitted into the atmosphere remains there. For example, it has been calculated that in the period 1958± 1968, enough fossil fuels were burned to increase the carbon dioxide content of the atmosphere by 1.24 ppm per year. The actual increase in CO2 content was 0.64 ppm=year. This is an indication of the enormous buffering effect of the earth's oceans on the CO2 concentration in the atmosphere. This buffering effect was discussed in Chapter 2 and is considered further in Sections 9.2.2 and 11.2.

3.3.4 Albedo Changes Changes in the earth's albedo have also been implicated in climate changes. Although large-scale cultivation, irrigation, damming of rivers to form lakes, and cutting down of forests all result in changes in the earth's albedo, these causes have heretofore been considered minor. The possible results of volcanic and other dusts in the atmosphere have, however, been investigated fairly extensively.

60

3.3 CAUSES OF GLOBAL CLIMATE CHANGES

Index of volcanic activity

Figure 3-15 shows an index of volcanic activity on earth between the years 1500 and 1970. Some of this volcanic activity was followed by worldwide cooling. For example, the ``Little Ice Age'' (1550±1850) occurred during a period of fairly high volcanic activity as well as low sunspot activity. Some of the highest peaks on Figure 3-15 are actually tremendous single volcanic explosions that were followed by noticeably cool years. The eruption of Asama in 1783 in Japan (the largest activity peak between 1700 and 1800 in Figure 3-15) was followed by three cool years, 1783±1785. The year 1816, called ``the year without summer'' (in New England, snow fell in June and there was frost in July), followed the eruption of Tambora, Sumbawa, in the Dutch East Indies in 1815. This eruption killed 5600 people and darkened the sky for days as far as 300 miles away. The large peak just before the year 1900 on Figure 3-15 is probably connected with the eruption of Krakatao in Indonesia in 1883. The eruption of Mount Agung in Bali in 1963, although not as spectacular as that of Tambora, occurred after accurate measurements of tropospheric temperature and aerosol measurements were being obtained, and is known to have resulted in a drop of 0.4 8C in the troposphere between latitudes 308S and 308N about one year later and lasting for about two years. It turns out that it is not the volcanic dust that contributes to tropospheric cooling, but aerosols consisting of submicrometer droplets of sulfuric acid derived from sulfurcontaining volcanic gases. Thus, the eruption of Mount St. Helens in the northwestern part of the continental United States in 1980 did not cause noticeable cooling because the gases released by this volcano contained only a small amount of sulfur. Volcanic ash falls out of the atmosphere within a few

2000 1500 1000 500 100 1500

1600

1700

1800

1900

1980

Year

FIGURE 3-15 Index of volcanic activity, in arbitrary units, that is proportional to the relative amount of material injected into the stratosphere in various 10-year periods. Redrawn from Inadvertent Climate Modi®cation Report of the Study of Man's Impact on Climate (SMIC). Copyright # 1971. Used by permission of MIT Press.

3. ENERGY AND CLIMATE

61

weeks or months, but the sulfuric acid aerosol droplets can remain in the stratosphere for years. The 1982 eruption of El ChichoÂn in Mexico apparently cooled the surface of the earth for several years because of the large amount of sulfuric acid aerosol formed afterward from sulfur-containing gases. The aerosols from the eruption of Mount Pinatubo in the Philippines and of Mount Hudson in Chile in 1991 apparently also caused global cooling for close to a year. It has been postulated that a large amount of dust and soot would be released into the stratosphere during a major nuclear war. For various reasons, this dust and soot would probably remain aloft for about one year. This would then increase the earth's albedo to the extent that considerable cooling of the earth would occur over several years. Calculations indicate that the earth could cool up to 18C for several years (recall that the difference between an ice age and an interglacial period is about 58C). This scenario has been called ``nuclear winter,'' and it includes major changes in precipitation and a probable depletion of the ozone in the stratosphere. Thus, this scenario includes a major disturbance of agriculture all over the earth in addition to depletion of the ozone layer that protects the surface of the earth from high-energy ultraviolet radiation.

3.3.5 Computer Models We have seen in Table 2-2 that humans are presently contributing a large amount of particulate matter, and, certainly, aerosols, to the atmosphere. If this material, like that emitted by volcanoes, can contribute to a cooling of the earth, presumably by increasing the earth's albedo, then this may partially mitigate the effects from the simultaneous CO2 emissions by humans. We have de®nitely been increasing both the carbon dioxide and the particle and aerosol content of the atmosphere, and these changes must have some in¯uence on the greenhouse effect and the albedo, which have a further effect on climate. Human efforts are superimposed on natural trends such as the orbital variations considered in the Milankovitch theory, but it is not clear at present whether human changes or natural effects have the greater magnitude. Furthermore, the earth's climate is determined by a complex set of positive and negative feedback systems that no one, at present, understands completely. As an example of a negative feedback (or self-limiting) possibility, suppose that an increase in CO2 content of the atmosphere caused an increase in temperature because of an increased greenhouse effect, which then caused an increase in evaporation of water from the oceans to form more cloud cover, which then re¯ected more of the sun's radiation to lower the temperature back toward its original value. It is an interesting exercise to dream up these self-limiting processes. The earth±atmosphere±ocean system is so complex that it is easy

62

3.3 CAUSES OF GLOBAL CLIMATE CHANGES

to imagine such self-limiting or even oscillating processes, but very dif®cult to develop models that produce results in which one has con®dence. A positive feedback possibility involves the idea of a slightly colder than usual winter with extra snow cover at high latitudes as postulated in the calculations made for Figure 3-12. This would increase the earth's albedo, allowing less of the solar radiation to heat the earth and its atmosphere than before; the extra snow would not melt completely. This would cause an even colder winter (because of the extra snow cover in the fall) in the following year, and so on. Good climate models need to invoke both negative and positive feedback systems. As we have seen, the earth's climate system is extremely complicated, so that computer models that can explore the consequences of any changes in the system must be quite simpli®ed. Figure 3-16 shows schematically the components of the earth's climate system that may or may not be considered in the various computer models of climate. Some computer models involve only energy balance for the earth as a whole, some involve the vertical distribution

Changes of solar radiation Space Atmosphere Terrestrial radiation Clouds

H2O, N2, O2, CO2, O3, etc.

Aerosols

Precipitation, evaporation

Air/biomass/ land coupling

Air/ice coupling Heat exchange

Ice

Ice/ocean coupling

Wind stress

Atmosphere/ocean coupling

Biomass

Land

Ocean

Changes of atmospheric composition

Changes of land features, orography, vegetation, albedo, etc.

Changes of ocean basin shape, salinity, etc.

FIGURE 3-16 Schematic illustration of the components of the earth's climate system, together with some physical processes responsible for climate change. Redrawn from M. C. MacCracken, A. D. Hecht, M. I. Budyko, and Y. A. Izrael. eds., Prospects for Future Climate. Lewis Publishers, Chelsea, MI. Copyright # 1990. Used with permission.

3. ENERGY AND CLIMATE

63

of temperature for the earth's surface and atmosphere (again, as a whole), and some involve the general circulation of the atmosphere and the oceans, allowing for the calculation of the geographical distribution of temperature, precipitation, and other climate quantities. These models are constantly being re®ned and checked against each other and against past climates of the earth. For example, a model developed at the National Center for Atmospheric Research (NCAR) in Boulder, Clorado, has given an excellent simulation of the present climate by incorporating the effects of ocean eddies hundreds of kilometers in diameter. This model has been used to predict a global warming from the increasing CO2 concentration in the atmosphere that is smaller than the amount anticipated by earlier models. Further comments are beyond the scope of this book.

3.4 SMALL-SCALE CLIMATE As we have seen, it is very dif®cult to ascertain what effects human activities may have had or will have on large-scale climate. However, human effects on small-scale climate are well known and worth discussing for that reason. Every town, every reservoir, every plowed ®eld changes the local climate to some extent. In this brief discussion of local climate, we shall con®ne ourselves to a consideration of urban climates, as distinguished from the surrounding countryside. On the average, urban climates are warmer and have more precipitation than the surrounding countryside. Table 3-3 compares an average city with the surrounding countryside for a number of climate elements. Note that a city is dirtier, cloudier, foggier, has more drizzly rain (precipitation days  5 mm total), more snow, less sunshine, less wind, and higher temperatures than the surrounding countryside. Wind speed is lowered in the city, except near very tall buildings, where appreciably higher wind speeds have been found in speci®c cases. The differences in temperature between a city and its surroundings can be much more variable than the Table 3-3 averages might imply. In London on May 14, 1959, for example, the minimum temperature was 528F (118C) in the city's center and 408F (48C) at its edges. In the period 1931±1960, however, mean annual temperatures for London were 11.08C (51.88F) at the city's center, 10.38C (50.58F) in the suburbs, and 9.68C (49.28F) in the adjacent countryside. Urban heat is generally assumed to arise from three causes. The most obvious source is the heat from combustion and general energy use in the city. A major cause of the warmer city nights is the release of heat stored in structures, sidewalks, streets, and so on in the daytime. A minor contributor to the warmth of cities is the back-re¯ection and reradiation of heat from pollutants in the atmosphere above the city.

64

3.4 SMALL-SCALE CLIMATE

TABLE 3-3 Microclimate of Urban Areas Compared with Surrounding Countryside Climate element Particulate matter Emitted gases Cloud cover Fog, winter Fog, summer Total precipitation Days with less than 5 mm Snowfall Relative humidity, winter Relative humidity, summer UV radiation, winter UV radiation, summer Sunshine duration Annual mean temperature Winter minimum temperature (average) Annual mean wind speed

Comparison with countryside 10 times more 5±25 times more 5±10% more 2 times more 30% more 5±10% more 10% more 5% more 2% less 8% less 30% less 5% less 5±15% less 0.5±1.08C higher 1±28C higher 20±30% less

Source: Reprinted from Inadvertent Climate Modi®cation, A Report of the Study of Man's Impact on Climate (SMIC). MIT Press, Cambridge, MA, 1971.

In the absence of winds, the pollutants in the atmosphere above a city often occupy a so-called urban dome (Figure 3-17), a sheath of air around the city that may be situated under a temperature inversion. The pollutants in an urban dome are reasonably well mixed, and the dome itself can often be distinguished from airplanes or from mountains near the city. Looking down on the urban dome of Los Angeles is something like observing a large pot of yellow pea soup! Urban domes have varying heights depending on conditions; an urban dome above a subarctic city in the winter may be only 100 m thick, while the dome over an oasis in the subtropics may be several kilometers thick. As we have noted, the urban dome tends to be warm; heat from combustion may supply up to 200 W=m2 , as in Moscow in the winter. When the wind blows, the urban dome becomes an urban plume, moving heat and pollutants downwind (Figure 3-18).

FIGURE 3-17 The urban dome.

65

3. ENERGY AND CLIMATE

Wind direction

FIGURE 3-18 The urban plume.

The existence of a visible urban dome implies different atmospheric composition over the city and in the surrounding country. The air over a city contains smoke, dust, SO2 , and so on, in much higher concentrations than country air. The particles in the air above the city increase the albedo above the city, thus reducing the intensity of the incoming solar radiation. In some cities, on bad days, the intensity of the incoming solar radiation may be reduced up to 50%. This means that cities tend to have cooler days than the surrounding country; these cooler days do not, however, make up for the warmer nights. The added particulate matter over cities also increases the frequency of fogs, since the particles can act as condensation nuclei for water vapor. The lower wind velocity in cities probably is caused by many obstacles (buildings) that are in the path of any wind in a city. The lack of standing water and the fast drainage of precipitation into storm drains result in a decrease of local evaporation and thus in the observed decrease of humidity in cities. However, when a city contains many cooling towers and there is generally a high water vapor output from burning of fossil fuels and industry, these factors, together with the extra condensation nuclei produced by the city, may cause an increased frequency of showers and thunderstorms downwind from the city and a weak drizzle within the city.

3.5 TEMPERATURE INVERSIONS When pollutants are trapped for a long time over a city, it is usually because of a temperature inversion above the city. This may result in accumulations that can reach lethal proportions, at least for the sick and elderly. Temperature inversions occur when air at some elevation in the troposphere ceases to decrease smoothly in temperature with increasing altitude as is normal near the surface of the earth (see later: Figure 3-20). At a temperature inversion, the air temperature increases with increasing altitude for a distance; at higher altitudes, the normal decrease in air temperature with increasing altitude begins again and continues up to the tropopause. The ways in which

66

3.5 TEMPERATURE INVERSIONS

such temperature inversions can occur will be discussed at the end of this section. To see why a temperature inversion traps pollutants, it is necessary to know what happens in the absence of such an inversion. In the daytime, the ground is heated by solar radiation, and the air near the ground is heated by conduction from the ground. The air, if we assume that it is an ideal gas, obeys the equation of state for ideal gases: PV  nRT

3-8

where P is the pressure, V is the volume of n moles of gas, R is the gas constant, and T is the absolute temperature. For our heated air, the pressure P of the atmosphere above it remains constant, but T increases. If we consider a ``packet'' of n moles of this air, and rewrite equation (3-8) as V  nRT=P, then we see that upon heating, V must increase, and the density, n=V, decrease. Consequently, this packet of air will rise until it reaches a place in the troposphere where the surrounding air has the same density; that is, the same temperature and pressure. Both the temperature and the pressure of the rising air packet change continuously as it moves to regions of lower pressure and therefore expands. The expansion can be assumed to be adiabatic; no heat ¯ows into or out of the packet during the process. Derivations of the equations for temperature and pressure changes in reversible adiabatic expansion of an ideal gas are given in most physical chemistry and many general chemistry textbooks. The result is P1 =P2  T1 =T2 Cp =R

3-9

where CP is the heat capacity at constant pressure of the gas, and subscripts 1 and 2 refer to properties of the gas before and after expansion, respectively. Qualitatively, this expression shows that if the gas is expanding, that is, if P2 < P1 , then T2 < T1 and the temperature of the gas will drop. This equation, together with the known decrease of pressure with height, allows calculation of the adiabatic lapse rate of dry air. This rate is a decrease of 18C for each 100 m, or 5.58F for each 1000 ft of altitude. The rising air cools faster than the temperature lapse rate of the environment, which involves a decrease of only 0.658C for each 100 m or 3.58F for each 1000 ft of elevation. Dry air will eventually rise to a height where temperature and, therefore, the density matches that of the surrounding air. If the rising air contains a lot of moisture that condenses as the air rises and becomes cooler, then heat is given off during this condensation and the air cools more slowly with height; that is, its temperature lapse rate is less than that of dry air. This moist air will therefore rise higher than dry air and will probably form clouds as it rises. These conclusions are illustrated in Figure 3-19 which shows what happens to heated dry air when the environment (the troposphere) is normal. The solid

67

3. ENERGY AND CLIMATE

line shows the temperature of the lower atmosphere when the temperature of the surface of the earth is 248C and there are no temperature inversions in the atmosphere. If the sun is shining, the surface of the earth absorbs heat and becomes warmer, heating the air just above it by conduction. The two broken lines in Figure 3-19 refer to two different ``parcels'' of air heated by the surface of the earth, to 25 and 268C, respectively. Both parcels of air will begin to rise as just discussed; they rise with the temperature lapse rate of rising dry air. Since the temperatures of these two parcels of air are decreasing faster, 18C per 100, than the temperature of the air through which they are rising, 0.658C per 100 m, each parcel will eventually reach a height at which its temperature equals that of the air already present. Its pressure and density are then also equal to that of the surrounding atmosphere, and the parcel will stop rising. Figure 3-19 shows that the parcel that was heated to 258C will rise to a height just below 300 m, while the parcel that was heated to 268C by the surface of the earth will rise to a height just below 600 m. Hotter air rises to a higher altitude. If a temperature inversion exists in the atmosphere at an altitude below that to which the heated air would normally rise, then the heated air may be trapped below the inversion, along with any pollutants that were present in the heated air. In Figure 3-20, which shows how heated air may be trapped when there is a temperature inversion in the troposphere, the solid line that

Height (m)

1000

500

1000 ft.

0 20

21

22

23 T (⬚C)

24

25

26

FIGURE 3-19 The fate of dry air heated by the earth's surface when the temperature lapse rate of the environment is normal: height vs temperature of the environment (solid line) and of rising, heated dry air (broken lines).

68

3.5 TEMPERATURE INVERSIONS

Height (m)

1000

500

0 20

21

22

23 24 T (⬚C)

25

26

27

FIGURE 3-20 How a temperature inversion traps heated air and its associated pollutants: height vs temperature of the environment (solid line) and of rising, heated dry air (broken lines).

shows the variation of atmospheric temperature with altitude is not linear; it has a region in which temperature increases with increasing altitude between approximately 400 and 600 m altitude. This region of increasing temperature is a temperature inversion; above and below this region the air exhibits its normal lapse rate of 0.658C per 100 m elevation. If the sun shines and the earth's surface is heated, the resulting ground-level heated air rises as shown by the broken lines in Figure 3-20. Three parcels of air are shown, one heated to 258C, the second to 268C, and the third to 278C. The parcel of air heated to 258C rises to the same altitude, just below 300 m, like the similar parcel in Figure 3-19; this happens because the temperature inversion occurs above this altitude and can affect only air that is attempting to rise through the inversion. Both the 268C and the 278C parcels of air are trapped by the inversion; each reaches an altitude at which its temperature equals that of the air already present within the temperature inversion zone. The 268C parcel of air rises to less than 500 m, considerably lower than the 600 m it would ordinarily reach (Figure 3-19). These temperature inversions that trap rising air are naturally occurring phenomena that may have two different causes. That is, they are of two different types, radiation inversions and subsidence inversions, explained in the following paragraphs. London tends to have radiation inversions in the winter; one of these trapped a highly polluted fog in 1952, producing the notorious London killer fog, which was considered responsible for over 3000 deaths. Los Angeles tends to have subsidence inversions that trap pollutants in the summer and fall.

69

3. ENERGY AND CLIMATE

Height (m)

1000

Subsiding air is heated. Lapse rate is the same as for rising air.

500

Inversion occurs at a height below that at which air ceased subsiding.

Original environment with normal lapse rate.

0

20

21

22

23 T (⬚C)

24

25

26

FIGURE 3-21 Mechanism by which a subsidence inversion occurs.

A radiation inversion generally occurs at night, when air near the ground is cooled by conduction from the cooled surface, especially on a clear night when radiation cooling occurs. Higher up in the troposphere, the air is not cooled appreciably, so, in the absence of winds, there is colder air underneath warmer air, an inversion by de®nition. A subsidence inversion occurs in a region where high altitude air is pushed down nearer the ground because of topographical features in the path of prevailing winds or weather systems. This air is being pushed to regions of higher pressure and therefore is being compressed adiabatically. The same equation that held for rising air also holds for this descending air, but now P2  P1 and T2  T1 ; that is, the air warms up as it nears the ground. Figure 3-21 shows how this subsiding air creates an inversion; again horizontal winds must be absent for the inversion to be reasonably stable. The two mechanisms for forming an inversion have exactly the same results, trapping of heated air and any pollutants that may be present. 3.6 CONCLUSIONS In this chapter, we have considered the climate history of the earth, the Milankovitch theory of the ice ages, the other factors that affect the earth's climate, the peculiarities of urban climate, and the formation and consequences of temperature inversions. It should now be possible to consider all the questions asked at the beginning of Chapter 2.

70

EXERCISES

The information presented in Chapters 2 and 3 shows how complicated the earth's atmosphere and climate are. Many of the discussion questions asked at the end of this chapter have no easy answers. In spite of this, newspapers and magazines often contain articles that present the problems of the possible control of the earth's climate by humans as if they were amenable to simple solutions. These chapters should make it possible to consider these articles and problems with consideration of their inherent complexity.

Additional Reading Berger, A., S. Schneider, and J. C. Duplessy, Climate and Geo-Sciences. A Challenge for Science and Society in the 21st Century. Kluwer Academic, Dordrecht, 1989. Boeker, E., and R. van Grondelle, Environmental Physics. Wiley, New York, 1995. Calder, N., The Weather Machine. How Our Weather Works and Why It Is Changing. Viking Press, New York, 1974. Gribbin, J., Forecasts, Famines and Freezes. Climate and Man's Future. Walker New York, 1976. Gribbin, J., Future Weather and the Greenhouse Effect. Delacorte Press, New York, 1982. Gribbin, J., ed., Climate Change. Cambridge University Press, Cambridge, U.K. 5 1978. Harries, J. E., Earthwatch. The Climate from Space. Horwood, New York, 1990. Houghton, J. T., G. J. Jenkins, and J. J. Ephraums, eds., Climate Change. The IPCC Scienti®c Assessment. Cambridge University Press, Cambridge, U.K., 1990. Hoyt, D. V., and K. H. Schatten, The Role of the Sun in Climate Change. Oxford University Press, New York, 1997. Inadvertent Climate Modi®cation. A Report on the Study of Man's Impact on Climate (SMIC). MIT Press, Cambridge, MA, 1971. JaÈger, J., and H. L. Ferguson, eds., Climate Change: Science, Impacts and Policy. Proceedings of the Second World Climate Conference. Cambridge University Press, Cambridge, U.K., 1991. Krause, F., W. Bach, and J. Koomey, Energy Policy in the Greenhouse. Wiley, New York, 1992. Lamb, H. H., Climate History and the Future. Princeton University Press, Princeton, NS, 1977. MacCracken, M. C., A. D. Hecht, M. I. Budyko, and Y. A. Izrael, eds., Prospects for Future Climate. A Special US=USSR Report on Climate and Climate Change. Lewis Publishers, Chelsea, MI, 1990. MacDonald, G. J., and L. Sertorio, eds., Global Climate and Ecosystem Change. Plenum, Press, New York, 1990. Peixoto, J. P., and A. Oort, Physics of Climate. American Institute of Physics, New York, 1992. Revkin, A., Global Warming. Understanding the Forecast. Abbeville Press, New York, 1992.

EXERCISES 3.1. How does the Greenhouse effect work (a) in a greenhouse and (b) in the earth's atmosphere? 3.2. The CO2 and CH4 content of the earth's atmosphere have been increasing steadily through this century. (a) What effect do most people think this will have on the earth's climate? Why? (b) Explain why your answer to part a might be wrong.

3. ENERGY AND CLIMATE

71

3.3. What are the three major factors that control earth's climate? Which of these factors may be affected by human activities? How? 3.4. What is an inversion? Explain how either a subsidence inversion or a radiation inversion occurs in the troposphere. 3.5. In 1997 some researchers made satellite measurements that indicated that the earth's polar regions are 0.558C warmer during a full moon than during a new moon. The same article mentioned that another researcher cautions that the effect may be an artifact caused by re¯ection of lunar light off a piece of the spacecraft (the satellite doing the measurement). From what you have learned about earth's climate, explain why you feel either (a) that the measurements are probably correct or (b) that they are probably an artifact and cannot be relied on. 3.6. (a) Which items usually considered in the heat balance of the earth would change appreciably if the earth were dry (no water present in any form): snow, ice, liquid, or vapor? Explain the increase or decrease in the items that change. (b) Would you expect a change in the mean temperature of the earth? Explain. 3.7. If all the earth's deserts were irrigated to produce crops of various kinds, what would be the effect, if any, on the earth's heat balance? Explain, and indicate whether you think the earth's mean temperature would increase, decrease, or remain the same. 3.8. Considering the increasing need for living space by the earth's ever increasing population, there have been proposals to try to make the northern latitudes more habitable by spreading many tons of soot or black dust on the Arctic ice sheet by cargo aircraft. This approach is expected to have the following results. Since the average thickness of this pack is about 3 m and it now shrinks by about 1 m during the summer melting season, the additional heat absorbed by a sooty surface might complete the melting of the ice in one or two seasons. The resulting open ocean would warm the lands on its border and also create more rainfall in an area that is now quite arid. (a) Is this proposal feasible? Why or why not? (b) Assuming that this proposal is feasible, what additional short-term results will it have? (c) What are some possible additional long-term results of this procedure, if it works? 3.9 The temperature lapse rate of the troposphere is 0.658C=100 m and the adiabatic lapse rate of dry air is 18C=100 m. Explain, with a diagram, the consequences if the temperature lapse rate of the troposphere were 1.18C=100 m.

4 PRINCIPLES OF PHOTOCHEMISTRY

4.1 INTRODUCTION Visible and ultraviolet solar radiation is essential for virtually all life on earth as we know it, and photochemical reactions are some of the most important processes taking place in the human environment. Several examples of photochemical in¯uences on our environment have already been given in Chapters 2 and 3. Direct utilization of solar energy as a possible alternative to fossil fuel combustion is discussed in Chapter 15, and its ef®cient usage is certain to be an increasingly important goal of research and development over the next few decades as we seek solutions for the worldwide energy problem. In Section 2.3.4 it is pointed out that atmospheric oxygen comes from photodissociation of water vapor in the upper atmosphere and from photosynthesis in the biosphere. Photosynthesis is a very important photochemical process that also leads to food production and storage of solar energy (Chapter 15). We discuss photochemical decomposition of petroleum, polymers, and PCBs and pesticides in Chapters 6, 7, and 8, respectively. Photochemical processes occurring at high altitudes in the mesosphere and stratosphere are essential for the maintenance of the thermal and radiation 73

74

4.1 INTRODUCTION

balance at the surface of the earth (see Chapter 3), and they also provide phenomena such as night glow. The reactions following light absorption in the lower atmosphere that generate photochemical smog from atmospheric pollutants are less desirable! In association with living matter, light-induced reactions lead to such phenomena as vision, cyclic activities of plants and animals, and both cellular damage and repair. In a more prehistoric context, it has been suggested that the origin of life may have occurred via the photochemical synthesis of purines, essential building blocks of nucleic acids. As we shall show later, absorption of light by a molecule results in excitation of the molecule to a higher electronic energy level. This is followed in many cases by reactions such as dissociation or interaction with other molecules, leading to the overall photochemical process. We shall see that the speci®c electronic state reached often determines the types of reaction that follow, so that the study of the absorption process is important to our understanding of photochemistry. In this chapter, we shall develop the basic principles of light absorption, electronic excitation, and subsequent photochemical and photophysical processes. As these principles are being developed, they will be applied to speci®c examples of photochemical processes occurring in our environment. Photochemistry is the study of the interaction of a ``photon'' or ``light quantum'' of electromagnetic energy with an atom or molecule, and of the resulting chemical and related physical changes that occur. The energy necessary for the reaction (or at least for it to be initiated) is thus gained from the photon. This is in contrast to thermal reactions, in which the energy needed for the reaction is distributed among the molecules and among the internal vibrational and rotational motions of the molecule according to the Boltzmann distribution law (Figure 4-1). As an example, consider the possible thermal dissociation reaction of molecular oxygen, O2 ! 2O

…4-1†

The fraction of molecules with thermal kinetic energy equal to or greater than a ``threshold'' energy Ec is approximately equal to the Boltzmann factor Nc ˆe N

Ec =RT

…4-2†

where Nc is the number of molecules with energies equal to or greater than Ec , N is the total number of molecules, R is the gas constant, 8:314 J K 1 mol 1 , and T is the temperature in kelvin. The energy required to break an oxygen bond is 5.1 eV, which is equivalent to 492 kJ=mol:1 Equation 4-2 gives the fraction of O2 1

The electron-volt (eV) is the energy required to move an electron through a potential difference of one volt; it is equal to 1:602  10 19 J, or 96.49 kJ=mol.

75

4. PRINCIPLES OF PHOTOCHEMISTRY

Fraction

0.03

0.02

0.01

20

40 Energy, E (kJ/mol)

60

80

FIGURE 4-1 Distribution of kinetic energy for O2 at 1500 K, expressed as the fraction of O2 molecules having energies between E and (E  1) kJ=mol.

molecules with energies Ec equal to or greater than 5.1 eV at 1500 K to be approximately 7  10 18, which is too small to lead to even the most ef®cient thermal reactions involving oxygen atoms. Many reactions such as this one that are not feasible thermally can, however, be initiated by light, as will be shown.

4.2 ELECTROMAGNETIC RADIATION 4.2.1. Properties of Light Monochromatic light is an electromagnetic wave of wavelength l traveling at speed c … ˆ 3:0  108 m=s in a vacuum) and having a frequency n equal to c=l. One of the important characteristics or properties of an electromagnetic wave for photochemical purposes is that it can transport energy, as it does for example from the sun to the earth or from a lightbulb to an object. In addition, an electromagnetic wave can transport momentum, hence is capable of exerting a radiation pressure. Although so small that we do not ordinarily feel it, this radiation pressure has been measured under very carefully

76

4.2 ELECTROMAGNETIC RADIATION

controlled conditions and is in complete agreement with classical theories of electromagnetic radiation. Most of the experimental techniques used in photochemistryÐpolarization, prisms and gratings to produce monochromatic light, and so onÐare based on the wave properties of light. It turns out, however, that many aspects of radiation, particularly its absorption and emission, are not adequately explained in this manner. Examples are the photoelectric effect and blackbody radiation, described in Section 3.1.1. The development of the Planck quantum hypothesis (1901), which was necessary to resolve these failures of the classical wave theory, led to the concept of the dual nature of matter and radiation and the theory of quantum mechanics. In essence, quantum theory says that energy interacts with molecules only in discrete amounts rather than continuously, so that a light beam may be considered to be made up of a stream of discrete units (photons or quanta). Each photon has zero rest mass and possessesÐand thus transportsÐa packet, or quantum, of energy e given by the Einstein relationship e ˆ hn ˆ

hc 

…4-3†

and momentum p pˆ

h 

…4-4†

where l is the wavelength of the corresponding electromagnetic wave and h is Planck's constant, a universal natural constant equal to 6:63  10 34 J
s. Referring back now to the energetics of the oxygen dissociation reaction [equation (4-1)], it is easily shown from equation (4-3) that the bond dissociation energy of 492 kJ=mol corresponds to a wavelength of 243 nm: ˆ ˆ

hc e …6:63  10

34

J
s†…3  108 m=s†…6:02  1023 mol 1 †…109 nm=m† …492 kJ=mol†…1000 J=kJ†

ˆ 243 nm

…4-5†

Thus when one photon of light having a wavelength of 243 nm is absorbed by an oxygen molecule, it will have suf®cient energy to break apart or dissociate. Table 4-1 gives the energy e of a photon and of an einstein of photons for several wavelengths and energy units.2 2

An einstein is one mole (6:022  1023 ) of photons.

77

4. PRINCIPLES OF PHOTOCHEMISTRY

TABLE 4-1 Photon Energies at Various Wavelengths Photon energy, e Wavelength 1m 1 cm (10 2 m) 1 mm…10 6 m† 1 nm (10 9 m 1 AÊ (10 10 m) 1 pm (10 12 m)

J=photon 2:0  10 2:0  10 2:0  10 2:0  10 2:0  10 2:0  10

25 23 19 16 15 13

kJ=einstein 1:2  10 4 0.012 120 1:2  105 1:2  106 1:2  108

eV 1:24  10 6 1:24  10 4 1.24 1:24  103 (1.24 keV) 1:24  104 (12.4 keV) 1:24  106 (1.24 MeV)

4.2.2 Absorption of Light The rather simple example just presented can be used to point out one of the basic principles of photochemistry (the Grotthus±Draper law, ®rst formulated early in the nineteenth century): for light to be effective in producing photochemical transformations, not only must the photon possess suf®cient energy to initiate the reaction, it must also be absorbed. Thus, even though we see from equation (4-5) that a 243-nm photon possesses enough energy to break the oxygen bond, in fact oxygen is not dissociated to any measurable extent when exposed to light of this wavelength because it is not absorbed. A second important principle of photochemistry, which follows directly from quantum theory, is that absorption of radiation is a one-photon process: absorption of one photon excites one atom or molecule in the primary or initiating step, and all subsequent physical and chemical reactions follow from this excited species.3 This principle is not strictly obeyed with the extremely high intensities possible from high-energy arti®cial light sources such as ¯ash lamps or pulsed lasers. When such high-intensity radiation is used, the simultaneous absorption of two photons is possible. However, only single-photon absorption occurs in all environmental situations involving solar radiation. In principle, electromagnetic radiation can extend essentially over an almost in®nite range of wavelengths, from the very long wavelengths of thousands of miles and low energies [the relationship between the two given by equation (4-3)] to the very short wavelengths of 10 12 m, which is on the order of magnitude of nuclear dimensions. It is convenient to divide this electromagnetic spectrum into regions, as given in Table 4-2. 3

As shown later, however, the overall effect from secondary reactions may be much greater than simply one molecule reacting per photon absorbed (see Section 4.4).

78

4.2 ELECTROMAGNETIC RADIATION

TABLE 4-2 The Electromagnetic Spectrum Spectral region Radio waves Microwave Far infrared (IR) Near IR Visible Near ultraviolet (UV) Far (vacuum) UV X-rays and g-rays

Wavelength range  10 cm 10 cm±1 cm 1 cm±0.01 cm 0.01 cm±700 nm 700 nm±400 nm 400 nm±200 nm 200 nm±100 nm < 100 nm

Energy range  1.2 J=einstein 1.2±12 J=einstein 12±1200 J (1.2 kJ)=einstein 1.2±170 kJ=einstein 170±300 kJ=einstein 300±600 kJ=einstein 600±1200 kJ=einstein > 1200 kJ=einstein

Photochemistry is generally limited to absorption in the visible, near-ultraviolet, and far-ultraviolet spectral regions, corresponding primarily to electronic excitation and (at suf®ciently high energies) atomic or molecular ionization. Absorption in different spectral regions may lead to different electronic states of the absorbing molecule and electronically different intermediate species, as well as to different products of the photochemical reaction. It is therefore important to understand the designations of electronic states of atoms and molecules insofar as they relate to or indicate possible electronic transitions and transition probabilities. A summary of the recipes used in arriving at atomic and molecular state descriptions is given in Appendix A; the mathematical formulations of these principles are given in standard textbooks of quantum mechanics and spectroscopy, some of which are given in the Additional Reading for Appendix A. Absorption in the low-energy radio, microwave, or infrared spectral regions results in no direct photochemistry unless very high-intensity laser radiation is used, the excitation for the most part only increasing the rotational and vibrational energies of the molecule and eventually being dissipated as heat. Some deleterious physiological effects do result from overexposure to microwave and infrared radiation (e.g., at radar installations or with improperly controlled microwave ovens), but these presumably are due to excessive localized heating. The chemical effects following illumination with very highenergy radiation (x-rays and -rays) are considered in Chapters 13 and 14. It is worth noting that there is concern about the health effects of electric and magnetic ®elds (EMFs), primarily in two categories: ELF-EMFs, or extremely low frequencies (mainly 60 Hz) from power lines, household appliances, electric blankets, etc., and RF-EMFs, or radio frequencies transmitted by cellular phone antennas (800±1900 MHz, the frequency range between UHF radio=TV and microwave ovens). Although ELF-EMFs can have biological effects at very high intensities, electric ®elds are so greatly reduced by

4. PRINCIPLES OF PHOTOCHEMISTRY

79

the human body that they are negligible compared with the normal body background electric ®elds; even the largest magnetic ®eld normally encountered (3000 milligauss) will not induce an electric current density comparable to that normally in the human body. Nevertheless, over the years several epidemiological studies have suggested fairly weak associations between exposures to ELF-EMFs, at levels found in typical residential areas, and some types of human cancers, particularly childhood leukemia.4 On the other hand, there are other recent epidemiological studies that ®nd no de®nitive link between typical ELF-EMF dosages and childhood leukemia.5 Reviews in recent years have also arrived at con¯icting conclusions. For example, one review strongly states that ``there is no conclusive and consistent evidence that ordinary exposure to ELF-EMFs causes cancer, neurobehavioral problems or reproductive and developmental disorders.''6 However, an advisory panel to the National Institutes of Health concluded that although there is a ``lack of positive ®ndings in animals or in mechanistic studies,'' ELF-EMF is a ``possible human carcinogen'' and should be classi®ed as such, and further strongly recommended that more research is needed.7 Many laboratory and epidemiological studies have also been carried out directed towards a possible link between RF-EMFs and brain cancer from handheld cellular phones where the antenna is placed near the head, even though they are operated at power levels ( 1W) well below which no known biological damage occurs. Most of these studies are controversial and inconclusive. However, the most recent (at the time of writing) reportsÐtwo case-control studies8 and one cohort study of almost half a million cell telephone subscribers9Ðclearly ®nd no association between cell phone usage and cancers of the brain. All agree, however, that risks associated with long-term exposures and=or potentially long induction periods cannot be ruled out. It is 4

For example, a highly cited reference is M. Feychting and A. Ahlbom, Magnetic ®elds and cancer in children residing near Swedish high-voltage power lines, Am. J. Epidemiol., 138, 467±481 (1993). 5 Such as M. S. Linet et al., Residential exposure to magnetic ®elds and acute lymphoblastic leukemia in children, N. Engl. J. Med., 337, 1±7 (1997); M. L. McBride et al., Power frequency electric and magnetic ®elds and risk of childhood leukemia in Canada, Am. J. Epidemiol., 149, 831±842 (1999), and correction, 150, 223 (1999). 6 National Research Council Committee on the Possible Effects of Electromagnetic Fields on Biologic Systems, Possible Health Effects of Exposure to Residential Electric and Magnetic Fields. National Academy Press, Washington, DC, 1997. 7 NIEHS Report on Health Effects from Exposure to Power-Line Frequency Electric and Magnetic Fields, NIH Publication No. 99±4493. National Institutes of Health, Bethesda, MD, 1999. 8 J. E. Muscat et al., Handheld cellular telephone use and risk of brain cancer, JAMA, 284, 3001±3007 (2000); P. D. Inskip et al., Cellular-telephone use and brain tumors, N. Engl. J. Med., 344, 79±86 (2001). 9 C. Johansen, J. D. Boice, Jr., J. K. McLaughlin, and J. H. Olsen, Cellular telephones and cancerÐA nationwide cohort study in Denmark, J. Natl. Cancer Inst., 93, 203±207 (2001).

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4.2 ELECTROMAGNETIC RADIATION

evident that continued long-term research is called for on the biological and biophysical effects from low-dosage exposure to ELF-EMFs and to RF-EMFs. Direct physiological and biochemical responses occur from exposure to ultraviolet light. Because of the characteristics of atmospheric ozone absorption (see Section 5.2.3) and the degrees of deleterious biological effects resulting from absorption in this spectral region, the near-ultraviolet region (400±200 nm) is often divided into three bands: UV-A (400±320 nm), UV-B (320±290 nm), and UV-C (290±200 nm). Generally speaking, the UV-C band is virtually totally absorbed by atmospheric ozone and the UV-A band, although transmitted by ozone, is not carcinogenic at reasonable exposure levels,10 so the UV-B bandÐpartially transmitted by atmospheric ozone (see later: Figure 5-4) and directly absorbed by speci®c molecules, such as DNA or proteinsÐis for the most part the biologically active one. The absorption of monochromatic electromagnetic radiation is given by the Beer±Lambert law, which says that the probability of light being absorbed by a single absorbing species is directly proportional to the number of molecules in the light path, which in turn is proportional to the concentration  (Beer's law) and the incremental thickness of the absorbing sample dx (Lambert's law) dI ˆ probability of light of intensity I being absorbed in thickness dx I ˆ fraction that the intensity I is reduced in thickness dx ˆ

ac dx

…4-6†

where a is the proportionality constant. The negative sign is included to account for the fact that the intensity is reduced by absorption, and thus dI is negative. Assuming that c and a are constant, integration of ac dx from the incident light intensity I0 at x ˆ 0 to I at x Z I Z I Z x dI ˆ d ln I ˆ ac dx …4-7† I0 0 I0 I leads to   I ˆ ln I0

acx

…4-8†

or I ˆe I0 10

acx

…4-9†

Radiation in the UV-A and visible regions has been implicated in malignant melanoma, possibly through energy or free-radical transfer from the broadly absorbing melanin. See R. B. Setlow, E. Grist, K. Thompson, and A. D. Woodhead, Wavelengths effective in induction of malignant melanoma, Proc. Nat. Acad. Sci. USA, , 6666±6670 (1993).

81

4. PRINCIPLES OF PHOTOCHEMISTRY

The absorbance A is I0 A ˆ log… † ˆ ecx I

…4-10†

where e … ˆ a=2:303† is the extinction coef®cient.11 The fraction of light absorbed is given by Ia ˆ1 I0

I ˆ1 I0

10

ecx

…4-11†

which holds for all concentrations. For small fractions of light absorbedÐfor example, at low concentrations of absorbers in the atmosphereÐthe fraction is directly proportional to the concentration of the absorbing species since e y  1 y when y is much less than unity: Ia ˆ1 I0

10

ecx

ˆ1

e

2:303ecx

 2:303ecx

…4-12†

This relationship cannot hold at high concentrations as is shown by going to the extreme in the opposite direction, where 2:303ecx is very large, so that essentially all the light is absorbed: Ia 1 I0

e

1

1

…4-13†

The light intensity I is normally expressed as the rate at which energy is transmitted through the cell or column of material, so that I0 is then the light energy incident at the cell face per unit timeÐthat is, it is the rate at which photons pass through the cell face. For reasons that will be apparent later, it is often convenient in photochemical systems to express the light absorbed, Ia, as the concentration of photons absorbed per unit time (photons volume 1 time 1 ) or alternatively of einsteins absorbed per unit time (einsteins volume 1 time 1 ). In these cases, I0 is then the concentration of photons or einsteins passing through the cell face per unit time. 1 The units of a and e are (concentration 1 length ), but obviously a variety of units may be used for concentration and length, leading to different values for a and e. If c is given in molarity M (mol=dm3 ) and x in centimeters, then a and e have the units M 1 cm 1 and e is called the molar extinction coef®cient, eM (sometimes referred to as the molar absorption coef®cient or the absorptivity). Frequently, however, in gaseous systems such as the atmosphere it is convenient to express the concentration in pressure units. These are generally related to concentration units at low pressures by the ideal gas equation 11 The constant a is also sometimes called the extinction coef®cient. In usage here, however, we shall always refer to the extinction coef®cient as the constant e in the Beer±Lambert law in the decadic (base 10) form, equation (4.10), and to a as the proportionality constant in equation (4-6).

82

4.2 ELECTROMAGNETIC RADIATION

P ˆ …n=V†RT ˆ cRT, and therefore the temperature must be speci®ed. If the pressure is to be expressed in atmospheres, R ˆ 0:08206 dm3 atm
K 1 mol 1 . If x is expressed in centimeters and the concentration of the absorbing species in molecules per cubic centimeter, as commonly used by atmospheric scientists, then the proportionality constant a in the base e form of the Beer± Lambert law, equation (4-8), has the units cm2 =molecule. This is called the absorption cross section and given the symbol s. For very strongly absorbing species, at maximum absorption s is roughly the order of magnitude of physical cross sections of molecules. In most cases we will use this absorption cross section and the symbol s for expressing the absorption curves. Table 4-3 summarizes and compares several of these Beer±Lambert law quantities for expressing the absorption of light by a single absorbing species. As a comparison of these various ways of expressing the proportionality constants, consider a hypothetical gaseous species at a pressure of 1 matm (10 3 atm) and 258C (298.15 K) that absorbs 40% of the incident light in 1 cm (i.e., is strongly absorbing). It follows from equations (4-9) and (4-12) that eM ˆ 5:43  103 M 1 cm a ˆ 1:25  104 M 1 cm

1 1

ˆ 222 atm 1 cm ˆ 511 atm 1 cm

1 1

and s ˆ 2:1  10

17

cm2 =molecule

Strictly speaking, the Beer±Lambert law applies only to monochromatic radiation, since e is a function of wavelength. The extent to which use of nonmonochromatic light leads to signi®cant error in the determination of concentration depends on the spectral characteristics of the absorbing and illuminating system. If the extinction coef®cient and incident intensity are known as functions of wavelength, however, the total amount of light absorbed may be obtained by integrating over all wavelengths. Also, if there are i absorbing species or components present, the Beer±Lambert equation in base 10 form [equation (4-10)] becomes

TABLE 4-3 Beer±Lambert Law Quantities Quantity A a e eM s

Name Absorbance Proportionality constant Extinction coef®cient Molar extinction coef®cient Absorption cross section

De®nition log10 …I0 =I† [lne …I0 =I†]/cx [log10 …I0 =I†]/cx [log10 …I0 =I†=c…mol=dm3 †x…cm† [lne …I0 =I†Š=c…molecules=cm3 †x…cm†

Units Unitless Concentration 1 length Concentration 1 length dm3 mol 1 cm 1 cm2 =molecule

1 1

83

4. PRINCIPLES OF PHOTOCHEMISTRY

I ˆ 10 I0

P

e i ci x

i

…4-14†

where the exponential part of the equation represents the sum of the ecx terms for all the i absorbing species.

4.3 KINETICS OF THERMAL PROCESSES Most chemical reactions are kinetically complex. That is, they take place by means of a series of two or more consecutive steps rather than by means of a single encounter of the reacting species. Nevertheless, the overall reaction between, say, two reactants A and B can be represented by the generalized equation aA ‡ bB ! cC ‡ dD ‡




…4-15†

where the stoichiometry of the reaction is given by the coef®cients a, b, c, d, . . . The rate, v, is then given by the differential equation vˆ

1 dnA ˆ a dt

1 dnB 1 dnC 1 dnD ˆ ˆ ˆ


b dt c dt d dt

…4-16†

where nA is the number of moles of A, nB is the number of moles of B, and so on, and dnA =dt is the change in the number of moles of A per unit time. For reactions in which the volume of the system (V) is independent of time, the molar concentration of A is ‰AŠ ˆ nA =V and d‰AŠ ˆ VdnA . Similarly, d‰BŠ ˆ VdnB , d‰CŠ ˆ VdnC , and d‰DŠ ˆ VdnD . It follows that the rate of the reaction per unit volume, r, usually referred to simply as the rate of the reaction, is rˆ

v ˆ V

1 d‰AŠ ˆ a dt

1 d‰BŠ 1 d‰CŠ 1 d‰DŠ ˆ ˆ ˆ


b dt c dt d dt

…4-17†

In certain cases it is convenient to express the rate with respect to the rate of change in concentration of a single reactant or product: rA ˆ rate of change of A ˆ

d‰AŠ d‰CŠ , rC ˆ rate of change of C ˆ , etc: dt dt …4-18†

However, it is important to remember that in general rA 6ˆ rC , although the two rates are related by the proportionality factor c=a. The expression for the experimentally determined rate of reaction in terms of the composition of the system can be quite involved. However, in many cases at constant temperature it is of the form r ˆ k‰AŠ ‰BŠ ‰CŠ ‰DŠ


‰XŠ




…4-19†

84

4.3 KINETICS OF THERMAL PROCESSES

where & is the temperature-dependent rate constant and X is neither a reactant nor a productÐthat is, it is a catalyst. The overall order of the reaction is the sum of the exponents a  b  g  d 


‡ x ‡


, and the order with respect to A is a, etc. For kinetically complex reactions there is in general no relationship between the exponents a, b, g, andd in equation (4-19) and the coef®cients a, b, c, and d in the stoichiometric equation (4-15). A special situation for equation (4-19) is the kinetically simple reaction that involves only the single step of reactants coming together. In this case the rate of the reaction at a given temperature is proportional only to the concentrations of the reacting speciesÐthat is, it does not depend on the nature or concentrations of the products of the reaction. The overall order of the reaction is then the number of reactant molecules (called the molecularity of the reaction) that must come together in a single encounter for the reaction to occur. Such reactions are called unimolecular, bimolecular, or trimolecular, depending on the number of reactant molecules; this number can be one, two, or three, respectively.12 Table 4-4 gives the rate expressions for the various possibilities of kinetically simple reactions. The integrated solutions of the corresponding differential equations [de®ned by equation (4-17)] for the rates of these kinetically simple reactions, leading to reactant concentrations as a function of reaction time t, can be obtained by standard integration techniques.13 These integrated forms are used to obtain reaction rate constants from experimental time-dependent concentration data. A chemically complex reaction is the combination of two or more kinetically simple steps, giving the mechanism of the reaction. We will encounter complex reaction mechanisms in Chapter 5 in connection with many physical and chemical interactions occurring in the troposphere and stratosphere. Simple differential equations can be written for each kinetically simple step in a mechanism; however, integration of the new combined differential equation becomes dif®cult and in most cases impossible by the usual analytical techniques, since products of one kinetically simple step generally become reactants in one or more other steps in the mechanism.14 Numerical methods 12

The probability that more than three molecules may come together in a single collision is so small that such events are not considered in kinetic treatments. 13 See C. Capellos and B. H. J. Bielski, Kinetic Systems. Wiley-Interscience, New York, 1972. k Two examples: For the unimolecular (®rst-order) reaction A ! product, we have 1 ‰AŠ k ˆ ln 0 ‰AŠ t

…4-20† k

and for the bimolecular (second-order) reaction A ‡ B ! product, we write kˆ

1 t…‰BŠ0

‰AŠ0 †

ln

‰AŠ0 ‰BŠ ‰AŠ‰BŠ0

…4-21†

14 Examples of some solutions of complex reactions are given by Capellos and Bielski (see note 13).

85

4. PRINCIPLES OF PHOTOCHEMISTRY

TABLE 4-4 Kinetically Simple Rates of Reaction I. Unimolecular (®rst-order) &

ˆ &‰AŠ A ƒƒ! products II. Bimolecular (second-order) & 2A ƒƒ! products

ˆ &‰AŠ2 & A ‡ B ƒƒ! products

ˆ &‰AŠ‰BŠ III. Trimolecular (third-order) & 3A ƒƒ! products

ˆ &‰AŠ3 & 2A ‡ B ƒƒ! products

ˆ &‰AŠ2 ‰BŠ & A ‡ B ‡ C ƒƒ! products

ˆ &‰AŠ‰BŠ‰CŠ

of integration are now possible for very complex mechanisms utilizing the tremendous computing power of present-day digital computers. Of course, justi®cation of a mechanism (or model) by computer simulation of this type requires good rate constants and spatial and temporal (space and time) behavior of all pertinent species. Two time quantities are sometimes used to describe the extent of a chemical reaction. One is the half-life, t1=2 , which is the time required for the reaction to be half-way completed; the other is the mean-life, t, which is the average of the lifetimes of all the reacting molecules. In general t1=2 and t depend on the concentrations of the species involved in the reaction. A unique case (and one k for which t1=2 and t are frequently used) is that of a ®rst-order reaction A ! products (such as radioactive decay; see Chapter 13), where it can be shown that t1=2 and t are independent of concentration: t1=2 ˆ

ln 2 0:693 ˆ k k

…4-22†

and tˆ

1 k

…4-23†

The mean-life t for a ®rst-order reaction is the time required for the concentration of the reactant to decrease to 1=e …1=2:718† of its initial value, in contrast to t1=2 , which is the time required for the concentration of the reactant to decrease to half of its initial value. The dependence of the rate on temperature is embodied in the rate constant k. The most useful relationship expressing this dependence is the empirical Arrhenius equation k ˆ Ae

Ea =RT

…4-24†

86

4.3 KINETICS OF THERMAL PROCESSES

or Ea RT

ln & ˆ ln A

…4-25†

In this treatment the preexponential factor A and the activation energy Ea are assumed to be temperature independent, so that from equation (4-25) a plot of ln k vs 1=T should be linear, with a slope equal to Ea =R. This behavior is found to be the case for many reactions, and this method involving the plot of ln k vs 1=T is the most common one for experimentally determining Ea . However, Arrhenius behavior will not necessarily be followed for kinetically complex reactions, and indeed reactions with very marked deviations from that predicted by equation (4-25) are encountered. The simple collision theory of chemical kinetics, applicable to kinetically simple bimolecular gas-phase reactions between two unlike hard-sphere species 1 and 2, considers the rate of reaction r … ˆ kc1 c2 † to be proportional to the frequency of bimolecular collisions Z12 . The proportionality constant equating r and Z12 includes the Boltzmann factor [equation (4-2)], which in this case is the fraction of molecules in two dimensions de®ned by the trajectories of motion of two colliding particles with energies equal to or greater than a potential energy barrier Ec. Note that this is the same form of exponential term found in the Arrhenius equation (4-24); the difference between the two is that Ea is the experimentally determined empirical activation energy, whereas Ec is associated with a speci®c potential energy barrier that must be overcome for the kinetically simple reaction to occur. The rate is also proportional to a temperature-independent steric factor p, which allows for the possibility that not all colliding particles with suf®cient energy to overcome the potential barrier do actually react. (For example, the molecules might not react unless they are in a particular orientation.) Thus, r ˆ pZ12 e

Ec =RT

ˆ kc1 c2

…4-26†

so that k ˆ p…

Z12 †e c1 c2

Ec =RT

ˆ pZ012 e

Ec =RT

…4-27†

where Z012 is the speci®c collision frequency and is proportional to T 1=2 . The preexponential term in the Arrhenius equation (4-24) is therefore slightly temperature dependent, and this is in fact observed for reactions with low or zero activation energies, although any small temperature effect in this term is completely masked by the exponential term for reactions with large activation energies. For small species such as atoms and diatomic molecules, Z12  2  10 10 cm3 molecule 1 s 1 . If the reaction goes at every collision (i.e., Ec ˆ 0, p ˆ 1), then k ˆ Z012 and is called the collisional rate constant.

87

4. PRINCIPLES OF PHOTOCHEMISTRY

A kinetically simple trimolecular gas-phase reaction requires the simultaneous encounter of three molecules. Collisions of this type (triple collisions) are very rare in comparison to binary collisions and are usually encountered only in two-body gas-phase combination reactions where simultaneous conservation of energy and momentum requires the presence of a third body. Trimolecular atom or small-radical combination processes in the presence of inert third-body molecules typically have triple-collision rate constants of the order of 10 32 cm6 molecule 2 s 1 . We will see several reactions of this type in Chapter 5.

4.4 KINETICS OF PHOTOCHEMICAL PROCESSES The second principle of photochemistry, that absorption is a one-photon process, taken together with quantum theory, requires that each quantum that is absorbed bring about a change (excitation) in that one molecule. In essence, this may be considered to be a ``bimolecular'' process involving interaction of one photon and one molecule. What happens to the excitation energy, however, depends on the amount of energy absorbed and the nature of the excited molecule. For example, the excited molecule can ``lose'' all or part of its excitation energy by transferring energy to another species via a nonreactive collision (collisional quenching), or it can emit energy in the form of a photon of light (¯uorescence or phosphorescence). Or, the excited molecule may undergo chemical processes (isomerize, dissociate, ionize, etc.), undergo chemical reactions with other species, or transfer its energy by collision to another molecule that ultimately results in a chemical transformation (sensitization). Thus, the overall number of molecules reacting chemically as a result of this absorption of a single photon may be virtually any value ranging from zero to a very large number ( 106 ). This latter is interpreted as arising from subsequent thermal chain reactions. We will encounter various reactions representing these physical and chemical processes in subsequent chapters. The ef®ciency of a photochemical reaction is the quantum yield. The overall quantum yield FJ of a substance J, which may be a speci®c reactant or a stable product, is simply the total number of the speci®c reactant molecules lost or stable product molecules formed for each photon absorbed. Thus, for the generalized reaction (4-15): number of A molecules reacted number of photons absorbed number of moles of A reacted ˆ number of einsteins absorbed

FA ˆ

and

…4-28†

88

4.4 KINETICS OF PHOTOCHEMICAL PROCESSES

number of C molecules produced number of photons absorbed number of moles of C produced ˆ number of einsteins absorbed

FC ˆ

…4-29†

Since A is the rate that A reacts, C is the rate that C is produced, and Ia by de®nition is the rate of light absorption, it follows that rA rC …4-30† FA ˆ , FC ˆ , etc Ia Ia This overall quantum yield FJ represents the overall ef®ciency of the reaction initiated by the absorption of light, which does not have to be absorbed explicitly by a reactant molecule. As already pointed out, however, the initial excitation act of absorption of a photon of light by a molecule X, hn

X ƒƒƒƒ! X

…4-31†

may be followed by a variety of physical and chemical primary processes (¯uorescence, deactivation, sensitization, etc.) involving the excited molecule X*. (Subsequent thermal chemical and physical reactions are considered secondary processes.) We can de®ne a primary quantum yield fi as the fraction of X* molecules undergoing a speci®c (ith) primary process. Thus, for ¯uorescence, f, in which light is emitted by an excited molecule, ff ˆ ˆ

number of X molecules emitting light number of photons absorbed by X

…4-32†

fluorescence rate r ˆ f rate of light absorption Ia

…4-33†

Thus, in general, for the ith primary process the rate ri is ri ˆ fi Ia

…4-34†

The symbol hn above the arrow in reaction (4-31) indicates that this is the light-absorbing reaction. Although this symbol should be used only for the kinetically simple light-absorbing step, it is often used even in the overall stoichiometric equation to signify a light-initiated reaction in which the overall mechanism consists of a complete set of primary and secondary processes. Since the energy of an absorbed photon has to go somewhere, to the extent that light absorption is a ``one-for-one'' event (the second principle of photochemistry), the maximum value for a single individual primary quantum yield is unity and the sum of all of the primary quantum yields for both physical and chemical processes must be unity: X fi ˆ 1 …4-35† i

4. PRINCIPLES OF PHOTOCHEMISTRY

89

where the summation includes all i modes of disappearance of the photoexcited species, including direct chemical reaction. Additional Reading Calvert, J. G., and J. N. Pitts Jr., Photochemistry. Wiley, New York, 1966. Gilbert, A., and J. Baggott, Essentials of Molecular Photochemistry. CRC Press, Boca Raton, FL, 1991. Logan, S. R., Fundamentals of Chemical Kinetics. Longman, Essex, U. K., 1996. Moore, J. W., and R. G. Pearson, Kinetics and Mechanism. 3rd ed. Wiley, New York, 1981. Suppan, P., Chemistry and Light. Royal Society of Chemistry, Cambridge, U. K., 1994. Turro, N. J., Modern Molecular Photochemistry. Benjamin=Cummings, Menlo Park, CA, 1978. Wayne, R. P., Principles and Applications of Photochemistry. Oxford University Press, Oxford, U. K., 1988.

EXERCISES 4.1. Ozone, O3 , is a weak absorber of electromagnetic radiation in the UV spectral region; its maximum absorption in the near ultraviolet region is at 255 nm. (a) Calculate the energy of a 255-nm photon in angstrom units (AÊ). (b) Calculate the energy of a 255-nm photon in joules per photon, in kilojoules per einstein, and in electron-volts. (c) Calculate the frequency of a 255-nm photon in reciprocal seconds and in reciprocal centimeters. (d) Calculate the momentum of a 255-nm photon in: kilogram-meters per second and in gram-centimeters per second. (e) How does the momentum of a 255-nm photon compare with the momentum of an ozone molecule at 258C moving at a velocity of 400 m=sÐthat is, what is Pphoton =Pozone ? 4.2. Give the spectral region in which each of the following photons might absorb: Ê -wavelength photon (a) a 5000-A (b) an 8-eV-energy photon (c) a 200-mile-wavelength photon (d) a 1013 -s 1 -frequency photon (e) a 5-cm-wavelength photon 4.3. Nitrogen dioxide (NO2 ) is a major participant in photochemical smog (Chapter 5). It absorbs visible and ultraviolet light, with maximum absorption at 400 nm, where its absorption cross section s is 6  10 19 cm2 =molecule. (a) Calculate its molar extinction coef®cient eM at 400 nm and its extinction coef®cient at 400 nm and 208C in units of atm 1 cm 1 .

90

EXERCISES

(b) Assume that the concentration of NO2 in a polluted atmosphere above a city is constant at 2  1012 molecules=cm3 to an altitude of 1000 ft and that the temperature is also constant at 208C. Calculate the percent of sunlight absorbed by the NO2 at 400 nm. 4.4. EDTA (ethylenediaminetetraacetic acid, MW 292.2) is an important industrial complexing agent (Section 9.5.6). It is poorly degraded in municipal sewage treatment plants and therefore is found in many surface waters. However, it forms a complex with the ferric ion (Fe3‡ ), Fe(III)EDTA, which can be photochemically degraded [F. G. Kari, S. Hilger, and S. Canonica, Environ. Sci. Technol., , 1008±1017 (1995)]. At 366 nm, the molar extinction coef®cient of Fe(III)-EDTA is 785 dm3 mol 1 cm 1 and the quantum yield of degradation is 0.034. In a sample of river water, the concentration of EDTA was found to be 280 mg=dm3 . (a) Calculate the fraction of light absorbed in 1-cm thickness (light path) of the river water sample at 366 nm if suf®cient ferric ion is added to complex all the EDTA. (b) The intensity of 366-nm sunlight is approximately 1014 photons cm 3 s 1 . Calculate the time required to degrade all the Fe(III)EDTA in one cubic centimeter of the sample in a cell 1 cm thick, assuming that the rate of the reaction does not change as the absorbing material is used up (a very poor assumption!). 4.5. We will see in Chapter 5 that the abstraction reaction of a hydrogen atom from an alkane molecule by an hydroxyl radical is an important initiating step in many atmospheric decomposition processes. This is a kinetically simple bimolecular reaction: k RH ‡ . OH ƒƒ! R. ‡ H2 O

At 298 K (258C), the rate constant k298 ˆ 6:9  10 15 cm3 molecule 1 s 1 for RH ˆ CH4. Assume that you could have a closed ¯ask containing initially methane and the hydroxyl radical at their estimated daytime concentrations in a typical polluted urban atmosphere: ‰CH4 Š ˆ 4:2  1013 molecules=cm3 and ‰. OHŠ ˆ 2:5  106 radicals=cm3 . (a) Calculate the initial rate of the reaction r, (b) Calculate the time required for half the
OH radicals in the ¯ask to be used up. (Hint: The initial concentration of methane is much greater than that of the hydroxyl radical, so the methane concentration can be assumed to be constant, giving an apparent ®rst-order reaction.) (c) Assume now that all sources of methane in the troposphere were suddenly stopped, but that the hydroxyl radical concentration remained constant. Calculate how long it would take for half the methane molecules to be used up, assuming that the foregoing reaction is the only one leading to the disappearance of methane.

5 ATMOSPHERIC PHOTOCHEMISTRY

5.1 INTRODUCTION We have already noted some of the important photochemical reactions occurring in the atmosphere that are important to the nature of our environment. In Section 2.3.4 we saw that photodissociation of water vapor in the upper atmosphere may be an important source of atmospheric oxygen. Molecular oxygen is photodissociated into oxygen atoms in the thermosphere, mesosphere, and upper stratosphere, and in so doing it absorbs most of the highenergy radiation below 180 nm. Ozone is produced in the stratosphere by the combination of an oxygen atom and an oxygen molecule. We saw in Section 2.5 that O3 extends the earth's shield against lethal ultraviolet radiation from 180 nm to about 290 nm. The troposphere connects the biosphere (i.e., the earth's surface) to the stratosphere and therefore is closely involved in the chemistry of both. For example, anthropogenic emissions of oxides of nitrogen and hydrocarbons, from internal combustion automobile engines and stationary furnaces, are major contributors to photochemical reactions in the troposphere that drastically affect the quality of our environment. Strong vertical mixing occurs in the troposphere, allowing species like methane and water that 91

92

5.1 INTRODUCTION

are produced naturally, as well as anthropogenic substances such as oxides of nitrogen and chloro¯uorocarbons, to be transported upward to contribute to photochemical processes occurring in the stratosphere. It is pointed out in Chapter 4 that while direct photochemistry is primarily limited to initiation by electronic excitation of the absorbing molecule, different electronic states can result from absorption in different spectral regions, which in turn may lead to different intermediate electronic species and chemical products. A summary of the methods for generating the designations (or term symbols) for atoms and simple molecules is given in Appendix A. The following is a brief summary of these state designations. The term symbol for an atom can be written in terms of atomic quantum numbers S, L, and J as …2S‡1†

LJ

where S represents the net (i.e., the resultant or vector sum) spin angular momentum (or simply the spin) of all the electrons of the atom; it can be zero or an integral number for an even number of electrons in the atom, or a half-integral number for an odd number of electrons. The quantity (2S ‡ 1) is called the multiplicity. The quantum number L describes the net electronic orbital angular momentum, and is given the symbols S, P, D, F, . . ., for the allowed values of L ˆ 0, 1, 2, 3, . . ., respectively. J is a quantum number designating the total angular momentum of the atomÐthat is, the vector sum of the spin (S) and orbital (L) angular momenta. For example, for an oxygen atom (eight electrons) in its lowest (ground) electronic state, S ˆ 1, L ˆ 1, and J ˆ 2, so the term symbol for the ground-state O atom is 3 P2 . For a diatomic molecule, the total term symbol is often given as …2S‡1† L…‡ or † …g or u†

where S and (2S ‡ 1) are the same as for atoms, L represents the total orbital angular momentum along the internuclear axis (analogous to L, L is given the symbols S, P, D, F, . . ., for L ˆ 0, 1, 2, 3, . . ., respectively), and (g or u) and (‡ or ) are associated with two types of symmetry operation that the diatomic molecule can undergo. States in which S ˆ 0, 1=2, and 1 (multiplicity ˆ 1, 2, and 3) are called singlet, doublet, and triplet states, respectively. For polyatomic molecules, in many cases it is suf®cient to designate an excited state in terms of the type of molecular orbital from which an electron is excited (the initial state) and the molecular orbital to which it is excited (the ®nal state). In addition, the multiplicity (2S ‡ 1) of the molecule is included in the designation. Speci®c examples are given in Appendix A.

5. ATMOSPHERIC PHOTOCHEMISTRY

93

Radiative absorption leading to transitions between electronic states (in contrast to collisional energy transfer) are limited by selection rules. The following rules give the allowed transitions:1 1. For atoms: (a) DS ˆ 0 ‰D(multiplicity) ˆ 0]; transitions where DS 6ˆ 0 are called spinforbidden (b) DL ˆ 0,  1 (c) DJ ˆ 0,  1, but J ˆ 0 ! J ˆ 0 is not allowed 2. For diatomic and light-nuclei polyatomic molecules: (a) DS ˆ 0 (b) DL ˆ 0,  1 (c) u !g; (d) ‡ ! ‡ and ! Sometimes we will use the complete designations to provide speci®c information about the states. In other situations, where a speci®c state is not key to our understanding of the system or the process being given, involvement of an electronically excited state generally is represented simply by an asterisk (*). If no designation is used, the species is in its ground electronic state.

5.2 REACTIONS IN THE UPPER ATMOSPHERE 5.2.1 Nitrogen We have seen that molecular nitrogen is the most prevalent species in the atmosphere. The reason that nitrogen is not so important photochemically is its large bond energy (7.373 eV, corresponding to a photon of wavelength l ˆ 169 nm), which limits its photodissociation chemistry to areas above the ozone layer. Molecular nitrogen absorbs only weakly between 169 and 200 nm, absorption in this leading to a spin-forbidden excitation from ground
region  state N2 to the 3 S‡ u excited state
 hn N2 ƒƒƒƒ! N2 3 S‡ …5-1† u 1

The selection rules are given here without proof or justi®cation, which can be found in standard quantum mechanics and spectra reference books, such as M. D. Harmony, Introduction to Molecular Energies and Spectra, Holt, Reinhart, & Winston, New York, 1972, pp. 450±455. Strictly speaking, these selection rules are valid (``allowed'' transitions) only for small molecules made up of light atoms; ``forbidden'' transitions can occur in larger molecules, particularly those containing heavy atoms, but they are generally of very low intensity.

94

5.2 REACTIONS IN THE UPPER ATMOSPHERE

that is a source of highly excited oxygen atoms by transfer of energy through collisions with ground-state O:

1  N2 3 S‡ …5-2† u ‡ O ! N 2 ‡ O S0

With photons of wavelengths below 100 nm, photodissociation occurs, possibly through photoionization and dissociative recombination involving ground-state O2 and producing nitric oxide (NO)2: hn …< 100 nm†

N2 ƒƒƒƒƒƒƒƒƒ! N‡ 2 ‡e N‡ 2

‡

‡ O2 ! NO ‡ NO ‡

NO ‡ e ! N ‡ O

…5-3† …5-4† …5-5†

An energetically excited nitrogen atom can be collisionally deactivated to the ground state by O2, producing singlet oxygen (discussed in the following section),
 N ‡ O2 ! N ‡ O2 1 Dg …5-6† or it can react with O2 to produce NO:

N ‡ O2 ! NO ‡ O

…5-7†

Nitric oxide might also be expected to form by direct combination of ground-state nitrogen and oxygen atoms, M

N ‡ O ƒƒƒƒ! NO

…5-8†

where M can be any other atomic or molecular species such as N, O, N2 , or O2 . This is a kinetically simple trimolecular reaction that occurs at essentially every triple collision between an N, an O, and an M species with a rate constant of the order of 10 32 cm6 molecule 2 s 1 (see Section 4.3). However, since photodissociation of N2 only occurs at high altitudes above the ozone layer where the total concentration of M is very small, this recombination reaction is not a signi®cant source of atmospheric NO. As we will see in Sections 5.2.3, 5.3.2, and 5.3.3, NO plays a signi®cant role in stratospheric photochemistry and it is also an important constituent in photochemical smog in the troposphere. At stratospheric heights it comes 2

NO has an odd number of electrons (15), and therefore one of them must be unpaired. This unpaired electron occupies an antibonding p orbital and is spread over the whole molecule. Nitrogen dioxide (NO2 ) also has an odd number of electrons (23) and thus also an unpaired electron, but in this case the electron is mostly localized on the N atom. Although NO and NO2 are technically free radicals and are involved in many free-radical reactions, in this book we will not indicate the lone (unpaired) electron on each of them as a dot; this will also be the case for atoms with odd numbers of electrons, such as hydrogen or the halogens. The dot will be used on other free radicals in this book.

95

5. ATMOSPHERIC PHOTOCHEMISTRY


 mainly from nitrous oxide, N2 O, by reaction with excited O 1 D2 oxygen atoms:
 N2 O ‡ O 1 D2 ! 2NO …5-9†

It is generally accepted that the N2 O is not produced directly in the atmosphere, but rather in the biosphere, primarily by microorganism reactions in soils and oceans (roughly two-thirds natural, one-third anthropogenic). Nitrous oxide is a strong greenhouse gas (Table 3-2). It does not react with the hydroxyl radical (. OH, the major initiator of removal of most trace gases in the atmosphereÐsee Section 5.3.2), nor does it absorb light above 260 nm, and therefore it is very stable in the troposphere. It is transported to the stratosphere primarily by large-scale movements of air masses within the troposphere. The concentration of N2 O in the atmosphere is now increasing above the preindustrial level at a rate of approximately 0.25%=year, due in large part to anthropogenic biomass burning and bacterial oxidation of fertilizer nitro3 gen (NH‡ 4 ). In addition to reaction (5-9), N2 O is destroyed in the stratosphere by photolysis. It absorbs light in a broad continuum starting at 260 nm, with a maximum at about 182 nm. The major photodissociation reaction is
 hn … 260 nm† N2 O ƒƒƒƒƒƒƒƒƒ! N2 ‡ O 1 D2

…5-10†

1

providing one stratospheric source of excited D2 oxygen atoms. Other sources are discussed in the following section.

5.2.2 Oxygen By far the most abundant photochemical reaction in the upper atmosphere is the photolysis of molecular oxygen. Figure 5-1 shows the potential energy curves for the various electronic states of O2 of importance to us; Figure 5-2 is the absorption spectrum in the far-ultraviolet and vacuum ultraviolet regions (note logarithmic absorption cross section vertical axis). It was shown in Section 4.2.1 that the bond dissociation energy of oxygen (5.1 eV, or 492 kJ=mol) corresponds to a photon of wavelength 243 nm. Oxygen actually begins to absorb just below this wavelength, at 242.2 nm, in a spectral region known as the Herzberg continuum. Absorption is very weak (s  10 23 cm2 =molecule at 202 nm), but the spectrum is a continuum in this region, indicating that dissociation occurs with f ˆ 1. Actually, excitation is to the weakly bound 3 S‡ u state (Figure 5-1, curve A) which rapidly dissociates into two ground-state atoms:   hn …< 242:2 nm†
 O2 3 Sg ƒƒƒƒƒƒƒƒƒ! O2 3 S‡ …5-11† u ! 2O 3

See Figure 10-6.

96

5.2 REACTIONS IN THE UPPER ATMOSPHERE

10

B

Potential energy (eV)

8

6

A 4

b 2

a x 0 0.09

0.115

0.14

0.165

0.19

0.215

0.24

0.265

0.29

0.315

Internuclear distance (nm) ‡

FIGURE 5-1 Potential energy curves for molecular oxygen. X ˆ 3 g , a ˆ 1
g , b ˆ 1 g , ‡ A ˆ 3 u , B ˆ 3 u . Drawn from data of F. R. Gilmore, J. Quant. Spectroscopy Radiat. Transfer, 5, 369±390 (1965).

10−16 10−17

(cm2/molecule)

10−18 10−19 10−20 10−21 10−22 10−23 10−24

120

140

160

180 200 Wavelength (nm)

220

240

FIGURE 5-2 Absorption spectrum of molecular oxygen (note logarithmic vertical axis). The dotted line is the Schumann-Runge banded region. Drawn from data of M. Ackerman, in Mesospheric Models and Related Experiments, G. Fiocco, ed., D. Reidel, Dordrecht, 1971, pp. 149±159.

97

5. ATMOSPHERIC PHOTOCHEMISTRY

The very weak absorption shown in this case is a good example of the consequence of selection rule violation, the speci®c one in this case being that excitation from a negative (superscript ) to a positive (superscript ‡) state is a forbidden transition. The other selection rules given in Section 5.1 for diatomic molecules are obeyed, however. Below 205 nm the absorption spectrum becomes much stronger and banded (the Schumann±Runge bands). The appearance of the banded spectrum rather than a continuum shows that absorption is now to a different potential energy curve from which dissociation no longer occurs at these energies. The Schumann±Runge bands get closer together as the wavelength decreases, and at 175 nm the bands blend together into a continuum known as the Schumann±Runge continuum which reaches maximum absorption at approximately 147 nm. Excitation in this Schumann±Runge region is to the bound 3 Su state, curve B of Figure 5-1:   hn …< 205 nm†
 …5-12† O2 3 Sg ƒƒƒƒƒƒƒƒƒ! O2 3 Su

This is an allowed transition, hence has a large absorption cross section (smax  1:5  10 17 cm2 =molecule). The 3 Su state dissociates at wavelengths shorter than 175 nm into one ground-state and one excited (1 D2 ) oxygen atom:   hn …< 175 nm†
 O2 3 Sg ƒƒƒƒƒƒƒƒƒ! O ‡ O 1 D2 …5-13†

The difference between the bond dissociation energy of O2 into two groundstate oxygen atoms (492 kJ=mol) and the start of the Schumann±Runge continuum (175 nm, corresponding to a photon energy of 682 kJ=einstein) is 190 kJ=mol, which is the energy needed to excite an oxygen atom from its ground (3 P2 ) state to the excited (1 D2 ) state. This is a large excitation energy, making the 1 D2 atom a very reactive and important species in stratospheric and tropospheric photochemistry. Below 130 nm there is suf®cient energy to produce oxygen atoms in even higher electronic states, and some dissociation to the 1 S0 state also takes place,
 hn …< 130 nm† O2 ƒƒƒƒƒƒƒƒƒ! O ‡ O 1 S0

…5-14†


 hn …< 92:3 nm† O2 ƒƒƒƒƒƒƒƒƒ! 2O 1 S0

…5-15†

and below 92.3 nm two excited atoms are produced

However, the ionization potential of O2 , 12.15 eV, corresponds to a photon of wavelength l ˆ 102 nm, and therefore a more likely reaction below 102 nm is photoionization hn …< 102 nm†

O2 ƒƒƒƒƒƒƒƒƒ! O‡ 2 ‡e

…5-16†

98

5.2 REACTIONS IN THE UPPER ATMOSPHERE

followed by dissociative recombination. Reactions (5-17) and (5-18) are two possible examples of this type of process:
1  O‡ …5-17† 2 ‡ e ! O S0 ‡ O ‡ 269 kJ=mol
1 
1  ‡ …5-18† O2 ‡ e ! O S0 ‡ O D2 ‡ 80 kJ=mol with (5-17) found to be the favored reaction. Two other excited electronic states of O2 are important in atmospheric photochemistry because of speci®c reactions to be discussed later with reference to their possible roles in the photochemical smog cycle, ozone photolysis, and photooxidation reactions with ole®ns. These are the 1 Dg (``singlet oxygen'') and 1 S‡ g states, with energies 94.1 and 157 kJ=mol, respectively, above the ground state (Figure 5-1). Direct excitation from the triplet ground state to either of these states is spin forbidden, and therefore oxygen absorbs only very weakly around 760 nm (157 kJ=mol), giving a banded spectrum called the atmospheric bands. The reverse radiative process is of course also spin forbidden and these states, when produced, are therefore relatively stable in the atmosphere, a factor contributing to their importance; the radiative 1 lifetime of 1 S‡ g is 12 s, while that of Dg is 60 min. Furthermore, nonreactive deactivation by collision with other species, called collisional quenching, is also inef®cient, the rate constants of deactivation by collision with groundstate O2 being 5  10 16 and 2  10 18 cm3 molecule 1 s 1 for the 1 S‡ g and 1 Dg states, respectively.4 In the absence of collisional quenching, the emissions from the normally ``forbidden'' radiative transitions   O2 1 S‡ …5-19† ! O2 ‡ hn…762 nm† g

and
 O2 1 Dg ! O2 ‡ hn…1270 nm†

…5-20†

turn out to be two of the most intense bands in the atmospheric airglow and in 1 auroral displays.5 The 1 S‡ g state also relaxes to the Dg state by collisional deactivation. Ground-state oxygen atoms can combine to form ground-state O2 by the three-body recombination reaction M

2O ƒƒƒƒ! O2

…5-21†

4 If deactivation occurred at every collision, the quenching rates would be approximately 4  105 and 108 times faster, respectively. See Section 4.3. 5 Airglow is the faint glow of the sky produced by solar photochemical processes; it occurs at all latitudes. The aurora is produced by impact of high-energy solar particles; it is more intense than the airglow, but it is irregular and occurs near the poles.

5. ATMOSPHERIC PHOTOCHEMISTRY

99

where M can be another oxygen atom or any other atomic or molecular species. If reaction (5-21) is kinetically simple and therefore trimolecular, then   r ˆ k‰OŠ2 M …5-22†

The rate constant k for this reaction is very nearly temperature independent. In fact it has a slightly inverse temperature behavior, the rate decreasing with increasing temperature, implying a negative activation energy, which of course is physically impossible if activation energy is considered to be the height of a potential barrier.6 The rate constant is also of the order of magnitude of the collisional frequency for triple collisions, indicating that the three-body recombination (5-21) occurs essentially at every encounter. Even so, at the very low pressures encountered in the upper atmosphereÐfor example, 3  10 7 bar at 100 km (see Table 2-4)Ðthe rate of reaction (5-21) is small compared to the rate of O2 photodissociation, and therefore above 100 km the primary oxygen species present is atomic oxygen.7 It has been seen that excited singlet (1 D2 and 1 S0 ) atoms are formed from the photodissociation of molecular oxygen below 175 nm. These species also relax to lower electronic states with emission of light:

 O 1 S0 ! O 1 D2 ‡ hn…557:7 nm† …5-25†
3 
1  …5-26† O D2 ! O P2 ‡ hn…630 nm†

Again, both are ``forbidden'' transitions and therefore show only weak emission contributing to the airglow and aurora. Below 140 km, however, collisional deactivation to the triplet ground state with any atomic or
molecu lar species M may become the dominant reaction, particularly with O 1 D2 . If

6 The reason for the negative activation energy is that oxygen atoms form an unstable intermediate complex with M, O. M, which then reacts with another O atom to produce O2 . As the temperature is raised, O. M becomes more unstable so that its concentration is decreased, thereby decreasing the rate at which O. M reacts with O, hence decreasing the overall rate of O2 formation represented by reaction (5-21). Since reaction (5-21) is now kinetically complex, as pointed out in Section 4.3.1, the interpretation of the experimental activation energy as the height of a potential energy barrier is not valid. Assuming equilibrium between O, M, and O. M leads, however, to the same rate law as that for the trimolecular reaction (5-22). At extremely high pressures, well beyond those in any part of the atmosphere, the order of the reaction would decrease from third order to second order. 7 It should be noted that radiative recombination processes are possible:  
 …5-23† ‡ hn 2O 3 P2 ! O2 1 S‡ g  
3 
1  O P2 ‡ O D2 ! O2 3 Sg ‡ hn 0 …5-24†

However, these reactions are also governed by spin conservation and atomic radiative selection rules, and they also are negligible in comparison to O2 photodissociation.

100

5.2 REACTIONS IN THE UPPER ATMOSPHERE

M is ground-state O2 , electronic energy is transferred and O2 is excited to its 1 ‡ Sg state  
 …5-27† O 1 D2 ‡ O2 ! O ‡ O2 1 S‡ g which decays collisionally to the 1 Dg state:  
 M O2 1 S‡ ƒƒƒƒ! O2 1 Dg g

…5-28†

An important aspect of this energy transfer or sensitization is that spin is conserved. That is, the oxygen atom undergoes a singlet±triplet transition while the reverse triplet±singlet reaction occurs with molecular oxygen, so that total reactant and product spins are the same. This is a very ef®cient process under exothermic conditions, probably occurring within an order of magnitude of collisional frequency, and reaction (5-28) is one of the
therefore  major sources of ``singlet oxygen'' O2 1 Dg in the atmosphere.

5.2.3 Ozone 5.2.3.1 Ozone in a ``Clean'' Stratosphere

Below 100 km into the midmesosphere region, the three-body recombination of O atoms, reaction (5-21), becomes potentially important because of the increasing total third-body pressure. However, the O2 concentration is also increasing as we go to lower altitudes, increasingly leading to absorption of the solar radiation below 243 nm. Photodissociation of O2 is decreased, lowering the O atom concentration. Since the rate of reaction (5-21) varies as the square of the O atom concentration (5-22), this three-body recombination becomes insigni®cant below the stratopause at approximately 50 km. However, another three-body recombination between a ground-state oxygen atom and a groundstate oxygen molecule to produce ozone     M O ‡ O2 ƒƒƒƒ! O3 ; r ˆ k O O2 M

…5-29†

does occur in this region [even though the trimolecular rate constant of (5-29) is less than that of reaction (5-21)] since it depends only linearly on the O atom concentration and the much higher O2 concentration.8 Reaction (5-29) is the exclusive source of ozone in the stratosphere and mesosphere (as well as being the only source of ozone in the troposphere, although the source of O atoms is different: see Sections 5.3.2 and 5.3.3), and

8

O and O3 are often referred to as ``odd oxygen,'' Ox .

101

5. ATMOSPHERIC PHOTOCHEMISTRY

is a major source of destruction of O atoms.9 Despite its small concentration (it does not exceed 10 ppm anywhere in the atmosphere), ozone is one of the atmosphere's most important and remarkable minor constituents. It is found throughout the atmosphere, but particularly in the stratosphere in a wellde®ned layer between 15 and 30 km altitude. Since its production depends on the photodissociation of molecular oxygen by the sun, it is produced primarily in the stratosphere near the equator and transported toward the Arctic and Antarctic poles.10 As pointed out in Chapters 2 and 3, not only does it provide the shield for the earth against damaging ultraviolet radiation, but also, through absorption of this radiation, it becomes the main energy reservoir in the upper atmosphere, hence a factor in climatic regulation. On the other hand, ozone is one of the most toxic inorganic chemicals known, and its presence at relatively high concentrations in lower atmosphere polluted air makes it a potentially dangerous substance for humans and other organisms. The bond dissociation energy of ozone is only 101 kJ=mol, corresponding to a photon of wavelength of 1180 nm, and the primary quantum yield of dissociation is unity throughout the visible and UV regions. However, ozone absorbs only weakly in the visible region (Chappuis bands), leading to ground-state species hn …visible†

O3 ƒƒƒƒƒƒƒƒƒ! O2 ‡ O

…5-30†

The wavelength of maximum absorption in the visible is 600 nm, smax  5:6  10 21 cm2 =molecule. The major absorption of ozone, known as the Hartley continuum (shown in Figures 5-3 and 5-4), is in the ultraviolet commencing at 334 nm with lmax ˆ 255:5 nm, smax ˆ 1:17  10 17 cm2 =molecule. This ultraviolet photolysis is quite complex, involving extensive secondary reactions. At wavelengths exceeding 310 nm, the predominant dissociative reaction is   hn …> 310 nm† O3 ƒƒƒƒƒƒƒƒƒ! O ‡ O2 1 Dg or 1 S‡ …5-31† g

but below 310 nm it is primarily



 hn …< 310 nm† O3 ƒƒƒƒƒƒƒƒƒ! O 1 D2 ‡ O2 1 Dg 9

…5-32†

It has been proposed that the reaction between a highly vibrationally excited ground-state oxygen molecule and another ground-state O2 molecule, and=or the reaction of a vibrationally and electronically excited 3 S‡ u oxygen molecule with a ground- state oxygen molecule, may also lead to the production of atmospheric ozone. See T. G. Slanger, Energetic molecular oxygen in the atmosphere, Science, 265, 1817±1818 (1994). 10 However, the ozone concentrations are about twice as large at the poles as at the equator because, until recentlyÐsee Section 5.2.3.2Ðthere were very few ozone-destroying reactions occurring at the poles.

102

5.2 REACTIONS IN THE UPPER ATMOSPHERE

15

(10−18cm2/molecule)

12

9

6

3

0

200

210

220

230

240 250 Wavelength (nm)

260

270

280

290

FIGURE 5-3 UV-C absorption spectrum of ozone at 298 K. Drawn from data of L. T. Molina and M. J. Molina, J. Geophys. Res., 91, 14,501±14,508 (1986).

1.5

(10−18cm2/molecule)

1.2

0.9

0.6

0.3

0

290

295

300

305 Wavelength (nm)

310

315

320

FIGURE 5-4 UV-B absorption spectrum of ozone at 298 K. Drawn from data of L. T. Molina and M. J. Molina, J. Geophys. Res., 91, 14,501±14,508 (1986).

103

5. ATMOSPHERIC PHOTOCHEMISTRY

and this is another primary source of singlet oxygen in the atmosphere.11 The several O2 and O3 photodissociation reactions just given may produce excited states of O and=or O2 as dissociation products, depending on the absorbed wavelengths. However, collisional deactivation of the excited states in general is so rapid even at stratospheric pressures that only the ground-state allotropic forms of oxygen (O, O2 , and O3 ) need to be considered in a natural or ``clean'' stratosphere.12 In the following we will therefore write the photodissociation reactions for O2 and O3 simply as hn …O2 †

and

O2 ƒƒƒƒƒƒ! 2O hn …O3 †

O3 ƒƒƒƒƒƒ! O ‡ O2

…5-36†

…5-37†

Total stratospheric formation of ozone is given by combination of reactions (5-29) and (5-36): hn …O2 †; M

3O2 ƒƒƒƒƒƒƒƒ! 2O3

…5-38†

This represents direct conversion of solar energy to thermal energy and leads to stratospheric heating. A tremendous amount of solar energy is involved: the average rate of energy conversion for the whole earth is greater than 2  1010 kJ=s (kW), which is over three times the total human rate of energy use. Ozone is destroyed by photolysis (5-37) and by reaction with ground-state O atoms 11 Recent studies [A.
 R. Ravishankara et al., Science, 280, 60 (1998) and included references] indicate that O 1 D2 atoms can be formed at wavelengths at least as great as 330 nm by the photolysis of internally excited (IE) ozone molecules, O3 (IE),



 hn …> 310 nm† O3 …IE† ƒƒƒƒƒƒƒƒƒ! O 1 D2 ‡ O2 1 Dg

and, to a much lesser extent, by the ``spin-forbidden'' (see Section 5.1) reaction  
 hn …> 310 nm† O3 ƒƒƒƒƒƒƒƒƒ! O 1 D2 ‡ O2 3 Sg 12

…5-33†

…5-34†

However, in a ``dirty'' that includes species other than just the oxygen allotropes
atmosphere  (e.g., water), singlet O 1 D2 atoms initiate many of the important free-radical reactions in the atmosphere, such as formation of the hydroxyl (. OH) radical:
 O 1 D2 ‡ H2 O ! 2. OH; k298 ˆ 4:3  10 12 cm3 molecule 1 s 1 …5-35†
1  The importance of the O D2 Ðproducing reactions above 310 nm given in footnote 11Ðis emphasized by the roughly threefold increase in solar intensity
 at sea level between 310 and 330 nm (Figure 3-4). Atmospheric reactions involving O 1 D2 atoms and the hydroxyl radical are covered in following sections.

104

5.2 REACTIONS IN THE UPPER ATMOSPHERE

[O3] (molecules/cm3) 1010

1011

1012

1013

80 Mesosphere Ozone

Altitude (km)

60

Temperature

40 Stratosphere 20 Troposphere 0 0

100

200 300 Temperature (K)

400

500

FIGURE 5-5 Atmospheric temperature and ozone concentration pro®les. Note that the ozone concentration axis is logarithmic.

O3 ‡ O ! 2O2

…5-39†

so that the total destruction in a ``clean'' stratospheric atmosphereÐcombination of reactions (5-37) and (5-39)Ðis hn …O3 †

2O3 ƒƒƒƒƒƒ! 3O2

…5-40†

Combination of the four reactions (5-29), (5-36), (5-37), and (5-39) is known as the Chapman cycle, proposed in 1930 as a theoretical explanation of the stratospheric ozone layer: hn…O2 †; M

3O2 ƒƒƒƒƒƒƒƒƒ! ƒƒƒƒƒƒƒƒƒ 2O3

…5-41†

hn…O3 †

This leads to a photostationary state13 in the stratosphere and at least qualitatively justi®es the temperature inversion at the stratopause, the temperature maximum at approximately 50 km, and the ozone concentration maximum at approximately 22 km (Figure 5-5). It should be emphasized, however, that stratospheric ozone concentrations also depend to a large extent on many physical factors, such as the latitudinal and zenith angle variations of the solar intensity and vertical and horizontal global air transport. It turns out 13

That is, a ``quasi-equilibrium,'' where the ratio of component concentrations is maintained constant as long as the light intensity is constant, giving the appearance of an equilibrium.

5. ATMOSPHERIC PHOTOCHEMISTRY

105

that stratospheric ozone is also affected by reactions involving species other than the three oxygen allotropes, even though these other species are present only in trace amounts, whereas huge quantities of ozone are produced and destroyed daily by the four reactions constituting the Chapman cycle. These reactions are discussed next.

5.2.3.2 Catalytic Destruction of Ozone in the Stratosphere

It has been pointed out before that the ozone layer is involved in stratospheric heating and control of the earth's climate, and in shielding the biosphere (the surface of the earth) from potentially dangerous near-ultraviolet radiation. In general, the lower the wavelength, and thus the higher the photon energy, the greater the direct biological damage. Exposure to solar radiation greater than 320 nm (the UV-A spectral region: see Section 4.2.2) at the earth's surface is not considered to be dangerous because DNA does not absorb above 320 nm. Radiation in the UV-C (200±290 nm) region is very damaging, but as we can see in Figure 5-3, ozone is a strong absorber in this region, and its concentration in the stratosphere is so high that virtually no UV-C radiation reaches the earth's surface. The critical region, then, is between 290 and 320 nm, the UV-B region, where the ozone absorption cross section is so low (Figure 5-4) that radiation is partially transmitted to the biosphere, and therefore the amount transmitted will vary with the ozone concentration. A general estimate is that a 1% decrease in the ozone concentration would lead to a 1.3% increase in UV-B radiation, although this is sensitive to the fraction of light transmitted, hence to the wavelength of the radiation. For example, at 290 nm a 1% decrease in ozone concentration would lead to a 10% increase in radiation at that wavelength, whereas at 320 nm the same decrease in ozone concentration would lead to only a 0.24% increase in radiation. It is important to note that the lower the wavelength, the more damaging is the radiation to DNA. Stratospheric ozone is maintained in a ``clean'' atmosphere by the ``quasiequilibrium'' reaction (5-41), by transport between the troposphere and the stratosphere, and by variable stratospheric winds. The amount of ozone continuously produced and destroyed daily in the stratosphere is so large that any signi®cant ``nonnatural'' overall destruction would require either an unrealistically large amount of ozone-destroying material or extremely ef®cient ozone-destroying reactions. In this section we consider several radical chain mechanisms or cycles in which the latter condition is met, thus suggesting that human activities could contribute (or have already contributed) to detectable modi®cations of the stratospheric ozone layer. Consider ®rst of all the reaction of nitric oxide with ozone. It was shown in Section 5.2.1 [reaction (5-9)] that NO is produced in trace amounts in the

106

5.2 REACTIONS IN THE UPPER ATMOSPHERE

stratosphere from N2 O. Nitric oxide destroys ozone in a direct reaction, producing nitrogen dioxide and an excited oxygen molecule: NO ‡ O3 ! NO2 ‡ O2

…5-42†

The rate constant for this reaction is very large. However, one molecule of NO is destroyed each time the reaction occurs, and its concentration in the stratosphere is very low relative to that of ozone, so that the fraction of O3 destroyed would be insigni®cant if this were the only process taking place. But the NO2 produced in reaction (5-42), reacts very rapidly with ground-state O to regenerate NO: NO2 ‡ O ! NO ‡ O2

…5-43†

The combination of reactions (5-42) and (5-43) is a chain mechanism, or cycle, NO ‡ O3 ! NO2 ‡ O2 NO2 ‡ O ! NO ‡ O2 net:

NO

O3 ‡ O ƒƒƒƒ! 2O2

…5-44†

in which the NO, called the chain carrier, leads to the destruction of O3 without being destroyed itselfÐthat is, it is a catalyst. Therefore, one NO molecule can lead to the destruction of a very large number of O3 molecules before it is eventually destroyed itself by a chain-terminating step.14 The possibility that this NO-catalyzed destruction could possibly lead to a signi®cant loss in stratospheric O3 was proposed in 1970.15 It is well known that jet aircraft, since they are air breathing, produce copious amounts of oxides of nitrogen, and it was projected at that time that a ¯eet of 500 transatlantic Concorde-type supersonic stratospheric transport (SST) aircraft ¯ying routinely at an elevation of 28 km could reduce the ozone layer by the order of 5%. For a variety of reasons (economic, political, and the 1970s oil crises) by 2000 the anticipated number of SSTs had not materialized (although second-generation supersonic planes called high-speed civil transports, HSCTs, are being considered for the twenty-®rst century), and as of now stratospheric NO comes predominantly from tropospheric N2 O (Section 5.2.1). 14

Note that reaction (5-44) is the same as the uncatalyzed ozone-destroying reaction in a ``clean'' atmosphere, reaction (5-39). 15 P. J. Crutzen, The in¯uence of nitrogen oxides on the atmospheric ozone content, Q. J. R. Meteorol. Soc., 96, 320 (1970).

107

5. ATMOSPHERIC PHOTOCHEMISTRY

Mechanism (5-44) is a typical catalyzed chain mechanism that can be generalized as follows: X ‡ O3 ! XO ‡ O2 XO ‡ O ! X ‡ O2 net:

X

O3 ‡ O ƒƒƒƒ! 2O2

…5-45†

Or, if the photolysis of ozoneÐreaction (5-37)Ðis included, the overall catalyzed destruction of ozone becomes X; hn

2O3 ƒƒƒƒ! 3O2

…5-46† 16

where X is a reactive odd-electron (see footnote 2) species. For mechanism (5-45) to compete with the corresponding uncatalyzed reaction (5-39), and therefore to signi®cantly lead to a reduction in stratospheric ozone, the two chain-propagating steps in the cycle must be very ef®cient. We see, for example, that the rate constants for these two steps in (5-44) at 298 K are 1:8  10 14 (5-42) and 9:5  10 12 …5-43† cm3 molecule 1 s 1 , respectively, both larger than the value of 8:4  10 15 cm3 molecule 1 s 1 for the uncatalyzed reaction (5-39). The rates of the individual reactions will of course depend on the concentrations of the several reacting species, in this case NO, NO2 , O3 , and O, which are dependent in a complex manner on many atmospheric chemical and physical parameters. For example, since mechanism (5-45) involves O atoms, it would be expected to decrease in importance at lower altitudes where the three-body reaction (5-29) that consumes O atoms is signi®cant. In general, mechanism (5-45) is considered to be signi®cant only above approximately 30 km, even though the maximum ozone concentration in the atmosphere, depending on latitude, is between 15 and 25 km. The radical that is considered to be the most signi®cant catalyst X in (5-45) in stratospheric ozone destruction is the chlorine atom, Cl. The primary sources of Cl atoms in the stratosphere, ®rst recognized in 1974,17 are the anthropogenic chloro¯uorocarbons, CFCs (Section 8.6). They are also potent greenhouse gases (see Section 3.3.3). CFCs are halogenated hydrocarbon gases. Chemically they are very inert and are relatively insoluble in water. Because of this inertness and their high volatility, they have found several key industrial usages, such as aerosol propellants, formation of plastic For example, besides NO, X could be H, . OH, Cl, Br, and so on. M. J. Molina and F. S. Rowland, Stratospheric sink for chloro¯uoromethanes: Chlorine atomic-catalyzed destruction of ozone, Nature, 249, 810±812 (1974); F. S. Rowland and M. J. Molina, Chloro¯uoromethanes in the environment, Rev. Geophys. Space Phys., 13, 1±35 (1975). Rowland and Molina, along with Crutzen (see footnote 15), shared the 1995 Nobel Prize in chemistry. 16 17

108

5.2 REACTIONS IN THE UPPER ATMOSPHERE

2.5

(10–18cm2/molecule)

2

1.5

1

0.5

0 150

160

170

180 190 Wavelength (nm)

200

210

220

FIGURE 5-6 Absorption spectrum of CFC-12 (CF2 Cl2 ). Drawn from data of C. Hubrich, C. Zetzsch, and F. Stuhl, Ber. Bunsenges. Phys. Chem., 81, 437±442 (1977).

foams, refrigerants, and electronic equipment cleansers. Their extreme inertness and insolubility in water also prevent them from being washed out of the atmosphere by rain, and for this reason as well, CFCs are very important in stratospheric ozone depletion. Long-term atmospheric monitoring of several CFCs, including the two most used ones, CFC-11 and CFC-12,18 at a variety of ``clean'' sites around the earth, has shown that their rates of systematic increase have been consistent with their anthropogenic worldwide production rates. This indicates that no major sinksÐthat is, physical or chemical methods of destruction or removal from the atmosphereÐexist for the CFCs within the troposphere. Thus, once released into the troposphere their only major loss is transport into the stratosphere by vertical movement of large air masses, which for the most part is independent of molecular weight. Once there, they may react with excited stratospheric oxygen atoms to produce reactive products such as Cl atoms and ClO. . More important, however, is that the CFCs absorb far-ultraviolet radiation, photodissociating with a quantum yield of unity into a chloro¯uorinated radical and a chlorine atom. For CFC-12, CF2 Cl2 ƒƒƒƒ! CF2 Cl. ‡ Cl hn

…5-47†

The ultraviolet absorption spectrum of CFC-12 is shown in Figure 5-6. Although radiation in this spectral region is completely prevented from reaching the troposphere by atmospheric oxygen and the ozone layer, it does partially penetrate into the stratosphere through the UV ``window'' between 18

See Table 3-2, note a, for a way of determining the formula of each gas from its number.

109

5. ATMOSPHERIC PHOTOCHEMISTRY

15 Oxygen

(10–18cm2/molecule)

12 Ozone 9 UV “window” 6

3

0 140

160

180

200 220 Wavelength (nm)

240

260

280

FIGURE 5-7 Solar UV window between oxygen and ozone absorption bands. Data for oxygen: 140±175 nm: M. Ackerman, in Mesospheric Models and Related Experiments, G. Fiocco, ed., D. Reidel, Dordrecht, 1971, pp. 149±159. 175±195 nm: K. Watanabe, E. C. Y. Inn, and M. Zelikoff, J. Chem. Phys., 21, 1026±1030 (1953). Data for ozone:  < 185 nm: M. Ackerman, in Mesospheric Models and Related Experiments, G. Fiocco, ed., D. Reidel, Dordecht, 1971, pp. 149±159.  > 185 nm: L. T. Molina and M. J. Molina, J. Geophys. Res., 91, 14,501±14,508 (1986).

approximately 180 and 220 nm formed by ozone and oxygen (Figure 5-7). Production of Cl atoms is then followed by the chain mechanism (5-45), with X ˆ Cl: Cl ‡ O ! ClO. ‡ O 3

2

ClO. ‡ O ! Cl ‡ O2 net:

Cl

O3 ‡ O ƒƒƒƒ! 2O2

…5-48† . If OH or NO is also present, additional catalyzed chain mechanisms involving atomic chlorine are possible. For example, with . OH, Cl ‡ O3 ! ClO. ‡ O2 . OH ‡ O ! HO . ‡ O 3

2

2

ClO. ‡ HO2 . ! HOCl ‡ O2 hn HOCl ƒƒƒƒ! . OH ‡ Cl net:

Cl; . OH; hn 2O3 ƒƒƒƒƒƒƒƒ! 3O2

…5-49†

110

5.2 REACTIONS IN THE UPPER ATMOSPHERE

and with NO, Cl ‡ O3 ! ClO. ‡ O2 ClO ‡ NO ! Cl ‡ NO2 NO2 ‡ O ! NO ‡ O2 net: or

Cl; NO

O3 ‡ O ƒƒƒƒƒƒ! 2O2

…5-50†

Cl ‡ O3 ! ClO. ‡ O2 NO ‡ O3 ! NO2 ‡ O2 ClO. ‡ NO2 ƒƒƒƒ! ClONO2 M

ClONO2 ƒƒƒƒ! Cl ‡ NO3 . hn

NO3 . ƒƒƒƒ! NO ‡ O2 hn

net:

Cl; NO; hn

2O3 ƒƒƒƒƒƒƒƒ! 3O2

…5-51†

Note that mechanisms (5-49) and (5-51) do not involve atomic oxygen and therefore can occur at lower altitudes than (5-48) and (5-50). This is important in the massive destruction of stratospheric ozone over the earth's poles, discussed in Sections 5.2.3.3 and 5.2.3.4, as well as the important fact that HOCl and ClONO2 serve as ``reservoir'' molecules in mechanisms (5-49) and (5-51), respectively, for the reactive Cl and ClO. species. For the anthropogenic chloro¯uorocarbons to be major contributors to stratospheric ozone depletion, they must of course be the primary source of stratospheric chlorine atoms. Several ``natural'' sources, such as sea salt, burning biomass, and volcanoes, have been cited as depositing many times more chlorine into the atmosphere than the CFCs, suggesting that ``natural'' chlorine atoms have been continuously contributing to the ozone photostationary state existing in the stratosphere to a much greater extent than could possibly be attributable to perturbation by anthropogenic chlorine atoms. Several observations contradict this proposal. For one thing, natural chlorine-containing species are for the most part water soluble (unlike the CFCs), and therefore if they are emitted into the troposphere they will be rained out before they are transported into the stratosphere. Sodium is not detected in the stratosphere, also ruling out sea salt. Biomass burning produces methyl chloride,19 but 19

See Section 10.6.13.

111

5. ATMOSPHERIC PHOTOCHEMISTRY

recent estimates put the contribution of methyl chloride from biomass burning to the total amount of stratospheric chlorine at about 5%. Active volcanoes can discharge HCl (and, to a lesser extent, HF) into the lower atmosphere. However, in the troposphere volcanic HCl rapidly dissolves in water (which is in large excess) after it has condensed to a supercooled liquid, so that for the most part the HCl is washed out by rain with only about 0.01% of that emitted possibly getting to the stratosphere. Furthermore, the concentrations of HCl and HF would be expected to decrease with increasing height in the stratosphere if from volcanic sources; in fact, it is found that they actually increase at stratospheric altitudes20 where concentrations of CFCs simultaneously decrease because they are in the process of photodecomposition. Of course, volcanoes undergoing very violent reactions do have the potential to deposit large quantities of HCl directly into the stratosphere, which bypasses washing out by rain. A very signi®cant factor indicating that such large volcanic activity is not a major contributor to stratospheric chlorine is the series of global measurements that have been made since 1978 on the accumulation of HCl in the stratosphere. During that time there have been two major volcanic eruptions: El ChichoÂn in Mexico in April 1982, and Mount Pinatubo the Philippines in June, 1991, with the former releasing about 1.8 megatons (1 megaton ˆ 1012 g) and the latter 4.5 megatons of HCl into the atmosphere. In spite of these, stratospheric HCl has increased regularly with only a small ( 1.0 ppb above 50 km. 21 Volcanic eruptions can also temporarily affect the earth's climate; see Section 3.3.4. 22 Even in the absence of volcanic activity, SO2 is present in the stratosphere from oxidation of reduced compounds of sulfur from natural and=or anthropogenic sources (such as carbonyl sul®de, COS, which is suf®ciently stable in the troposphere to reach the stratosphere).

112

5.2 REACTIONS IN THE UPPER ATMOSPHERE

stratosphere for years. Enhanced heterogeneous chlorine-catalyzed, ozonedepleting reactions can take place on these aerosols, as discussed in the next section in conjunction with the Antarctic ozone hole. It has been found, in fact, that stratospheric ozone depletion is enhanced after large volcanic activity, such as Mount Pinatubo, by these surface reactions, but not by ejected HCl. The volcanic debris also absorbs sunlight (e.g., the sunlight was attenuated between 15 and 20% at several Northern Hemisphere measuring sites at the peak of the effect following the Mount Pinatubo eruption), increasing the temperature of parts of the stratosphere and possibly altering the high-altitude winds that circulate tropical ozone around the globe. Bromine atoms can also participate in the catalyzed mechanism (5-45): Br ‡ O3 ! BrO. ‡ O2 BrO. ‡ O ! Br ‡ O 2

net:

Br

O3 ‡ O ƒƒƒƒ! 2O2

…5-54†

Stratospheric bromine atoms come primarily from photolyses of methyl bromide (CH3 Br) and brominated CFCs (halons).23 Methyl bromide (Section 8.6.2.3) occurs naturally in the atmosphere, mostly from oceanic marine biological activity and from forest and grass (biomass) ®res.24 It is also synthesized for agricultural uses as a soil fumigant, and it is emitted into the atmosphere from automobile exhausts. The anthropogenic halons, mainly H-1301 and H-1211, are used extensively for extinguishing or suppressing ®res. Methyl bromide is rapidly degraded by soil bacteria; most of it released into the atmosphere is taken up by the oceans or is oxidized or photolyzed in the troposphere, but an appreciable amount does reach the stratosphere. The total concentration of bromine in the lower stratosphere is approximately 19 parts per trillion by volume (pptv). There are no known effective stratospheric reservoirs for Br or BrO., unlike Cl and ClO. which have HOCl [mechanism (5-49)] and ClONO2 [mechanism (5-51)], respectively. As a result, Br atoms are about 50 times more destructive of ozone than Cl atoms on a per-atom basis, although overall Cl atoms are more destructive because of the much greater concentration of Cl-containing compounds in the stratosphere than Brcontaining compounds. In addition, ozone depletion by chlorine atoms is enhanced by bromine atoms through a synergistic interaction involving coupling of the BrO. and ClO. cycles:

23

Halons are designated as H-wxyz, where w, x, y, and z are the number of carbon, ¯uorine, chlorine, and bromine atoms, respectively. Thus, CF3 Br is H-1301, and CF2 BrCl is H1211. 24 However most of these are deliberately set and thus are anthropogenic in origin.

113

5. ATMOSPHERIC PHOTOCHEMISTRY

BrO. ‡ ClO. ! Br ‡ ClO2 . ClO2 . ƒƒƒƒ! Cl ‡ O2 Br ‡ O ! BrO. ‡ O M

3

2

Cl ‡ O3 ! ClO. ‡ O2 net:

Cl; Br

2O3 ƒƒƒƒ! 3O2

…5-55†

It is estimated that at the time of writing approximately 25% of the global stratospheric ozone destruction is caused by bromine. The depletion of ozone by a halogen-containing hydrocarbon depends on several factors, including the rate at which the hydrocarbon enters the atmosphere and its lifetime in the atmosphere (i.e., the time required for a given amount of a substance emitted ``instantaneously'' into the atmosphere to decay to 1=e of its initial value). The atmospheric lifetimes of fully ¯uorinated (per¯uoro) gaseous compounds are very long (many centuries), since their loss results primarily from photolysis in the mesosphere, where pressures are very low and mixing with lower-altitude gases is extremely slow. Partial chlorination (CFCs) or bromination (halons) shortens the lifetime because of absorption and photolysis in
the 180 to 220-nm UV window (Figure 5-7), as well as destruction by excited O 1 D2 atom reactions, both processes occurring in the stratosphere. Replacing some of the halogens with hydrogen or incorporating unsaturation in the molecule further greatly shortens the atmospheric lifetime because of reactions, such as with the . OH radical, in the troposphere. Atmospheric lifetimes of several halogenated gases are given in Table 5-1. A factor that quanti®es the ability of a gas to deplete stratospheric ozone is the ozone depletion potential (ODP), which is the steady-state depletion of ozone calculated for a unit mass of a gas continuously emitted into the atmosphere relative to that for a unit mass of CFC-11. Examples of ODPs are also given in Table 5-1. One-dimensional (1-D) and two-dimensional (2-D) models are used in the calculations of ODPs. (The ODPs in Table 5-1 are based on 2-D models.) Both types of model include modes of transport of atmospheric species, absorption and scattering of solar radiation, and approximately 200 chemical reactions involving about 50 reactive species; the difference between the two models is that the 1-D models consider only vertical distribution of species, assuming constant horizontal averages, whereas the 2-D models consider vertical and north±south (latitudinal) changes, but not east± west (longitudinal) effects. Major contributions to the uncertainties in the ODPs are the steady-state assumption and the lack of inclusion of the processes that produce the Antarctic ozone hole. Therefore the ODPs should be considered only as estimates to give a general picture of the effects of various constituents in halogenated gases. Table 5-1 lists the lifetimes and ODPs for

114

5.2 REACTIONS IN THE UPPER ATMOSPHERE

TABLE 5-1 Range of Lifetimes and Ozone Depletion Potentials (ODPs) of Selected Halogenated Gases Compound CFC-11 CFC-12 CFC-113 HCFC-141b HCFC-142b HCFC-22 HFC-134a HFC-152a H-1301 H-1211 CF4 CH3 Br CF3 I HFE-7100

Lifetime (years) 50 102 85 9.4 19.5 13.3 14 1.5 65 20 >50,000  1:3 < 2 days 4.1

ODP 1.0 0.82 0.90 0.10 0.05 0.04 < 1:5  10 0 12 5.1 0  0:6 0 0

5

Source: Scienti®c Assessment of Ozone Depletion: 1994, World Meteorological Organization Global Ozone and Monitoring Project, Report No. 37, U. S. Department of Commerce (1995). Data for the hydro¯uoroether HFE-7100 (C4 F9 OCH3 Ðsee Section 5.2.3.5) is from J. G. Owens, ``Low GWP Alternatives to HFCs and PFCs,'' presented at the Joint IPCC=TEAP Expert Meeting on Options for the Limitations of Emissions of HFCs and PFCs, Energieonderzoek Centrum Nederland, Petten, The Netherlands, 1999.

selected CFCs, HCFCs, HFCs, and halons that together account for more than 95% of the organic chlorine and more than 85% of the organic bromine in the atmosphere in 1995.25 The very large ODPs for the halons are due primarily to the synergistic coupled BrO. and ClO. cycle, mechanism (5-55). CFCs were ®rst developed in 1930, and as pointed out earlier, until recently they (and the later developed halons) were used extensively in applications that could bene®t from their inertness, volatility, and safety. It is estimated that approximately 90% of all the CFC-11 and CFC-12 produced to date has now been released into the troposphere. But has the release of CFCs and halons into the atmosphere already depleted the stratospheric ozone layer to a measurable extent? 25 S. A. Montzka et al., Decline in the tropospheric abundance of halogen from halocarbons: Implications for stratospheric ozone depletion, Science, 272, 1318±1322 (1996).

5. ATMOSPHERIC PHOTOCHEMISTRY

115

To try to answer this question, we ®rst consider how atmospheric ozone concentrations are experimentally measured. The Dobson spectrophotometer, in use since 1926, determines the total ozone contained in a vertical column passing through the earth's atmosphere. It does this by measuring the amount of radiation from the sun (or re¯ected from the moon) that is absorbed by the ozone at a pair of wavelengths near 300 nm. Currently there are more than 140 Dobson spectrophotometer operating stations positioned around the globe, forming the Global Ozone Observing System (GO3 OS). A similar groundbased instrument is the M-124 ®lter ozonometer; instead of a spectrophotometer, however, it uses two wideband optical ®lters, with maximum spectral sensitivities at 314 and 369 nm. Located at more than 40 sites (primarily in the former Soviet Union), these instruments also contribute to the GO3 OS network. Another ground-based or airborne system used to determine atmospheric ozone concentrations is ifferential bsorption idar (DIAL), which transmits light at two wavelengths, one that is at an ozone absorption line and is backscattered by ozone, and the other that is not at an ozone absorption (to correct for natural backscatter).26 In addition, ozone concentrations from the earth's surface to heights as high as about 30 km have been measured by electrochemical concentration cell ozonesondes, carried aloft by balloons. Total global coverage of ozone has also been measured since 1978 from above the atmosphere by a variety of instruments aboard polar- and precess-orbiting satellites. For example, the total ozone mapping spectrometer (TOMS) measures the ozone attenuation of six UV emissions from the earth between 312 and 380 nm. A similar UVscanning satellite instrument is the solar backscattered ultraviolet (SBUV or SBUV=2) spectrometer. The microwave limb sounder (MLS), aboard the Upper Atmospheric Research Satellite (UARS) launched in 1991, determines stratospheric ozone concentrations from its microwave thermal emission lines at frequencies 183 and 205 GHz (1 GHz ˆ 109 s 1 ). Satellites have also been used to determine the vertical atmospheric ozone concentration in the Stratospheric Aerosol and Gas Experiments (SAGE I, II, and III), and (since 1998) total ozone in the Global Ozone Monitoring Experiment (GOME). First of all, measurements from these sources from as long ago as the 1950s to 1980 gave an average total ``column'' ozone concentration of about 312 Dobson units (DU) in the Northern Hemisphere and 300 DU in the Southern Hemisphere, with an overall global average of approximately 306 DU over this time period.27 Superimposed on these averages, though, are periodic ¯uctuations 26

Lidar is essentially radar that uses lasers as sources of pulsed electromagnetic radiation. The Dobson unit is a measure of the total integrated concentration of ozone in a vertical column extending through the atmosphere. It is the pressure in milliatmospheres (matm: 1 matm ˆ 10 3 atm) that all the ozone in this column would have if it were compressed to one centimeter height. Thus, for 300 DU, the pressure of ozone in the hypothetical 1-cm column would be 300 matm. Assume now that the height of the column is increased to 30 km (3  106 cm) altitude 27

116

5.2 REACTIONS IN THE UPPER ATMOSPHERE

greater than 5%; these are due to seasonal variations (as much as 4% difference between a May±September maximum and a December minimum) and natural meteorological phenomena that include the tropical Quasi-biennial Oscillation (an approximately 26- to 27-month oscillation or cycle between easterly and westerly winds in the lower equatorial stratosphere), 11-year solar sunspot cycles and ¯uctuations, and the El NinÄo±Southern Oscillation of about 4 years (Section 3.3.1). Nevertheless, when the measurements over the 30-year period from 1964 to 1994 are treated and smoothed with a statistical model to ®lter out these natural components, they still show an overall global decline of approximately 4% in total ozone during the 13 years between 1978 and 1992, with however the change near the equator close to zero (Figure 5-8). About 64% of this total global change appears in the Southern Hemisphere. In 1992, beginning in May, the global total ozone concentration dropped about 1.5% lower than expected from a linear extrapolation of the rate just given. In December 1992, the ozone levels in the northern midlatitudes over the United States were about 9% below normal, dropping to about 13% below normal in January and continuing well below normal into July, 1993, getting to as low as 18% lower at some sites. Similar record low stratospheric ozone levels were also observed over Canada and eastern and southern Europe, extending through August, 1993. Smaller unexpected midlatitude decreases appeared in the Southern Hemisphere. These extraordinary and unprecedented effects are believed to have resulted from the June 1991 eruption of Mount Pinatubo, which increased the stratospheric sulfate aerosol layer. However, volcanic aerosols had essentially disappeared by mid-1993, and in fact the annual decrease in total ozone had returned in 1994 to the pre-1991 values. This is as predicted, as the stratosphere recovered from volcanic debris. at a constant temperature. (Over 90% of the ozone in the atmosphere is contained below 30 km.) Assuming ideal gas behavior, the average pressure of ozone within the column will now be 10 4 matm, since pressure is inversely proportional to volume (hence also inversely proportional to the height for a column of constant cross section) under these isothermal and ideal gas conditions. Note that the product Px, where P is the pressure and x the height of the cylindrical column of ozone, is independent of x. Thus, in this example,

 Px ˆ 10 4 matm 3  106 cm ˆ …300 matm†…1 cm† ˆ 300 matm cm ˆ 300 DU

so that

1 DU ˆ 1 matm
cm ˆ 10

3

atm
cm:

This is useful if the concentration c in the Beer±Lambert law (Section 4.2.2) is expressed in terms of pressure P. For example, the absorption cross section (s) of ozone at 305 nmÐmidway in the UV-B bandÐis 2  10 19 cm2 =molecule, which converts to the base-10 extinction coef®cient e ˆ 2:14 atm 1 cm 1 at 298 K. The fraction of light transmitted through the atmosphere at 305 nm is then given by Equation 4.11 as I ˆ 10 I0

ePx

ˆ 10 …2:14 atm

1 cm 1

†…300 DU†…10

3

atm
cm=DU†

ˆ 0:228 ˆ 22:8%

117

5. ATMOSPHERIC PHOTOCHEMISTRY

4

Total ozone change (%)

2 0 –2 –4 –6 –8 –10 1964

35⬚N – 90⬚N 35⬚N – 35⬚S 35⬚S – 90⬚S

1968

1972

1976

1980 Year

1984

1988

1992

FIGURE 5-8 Percent change in total ozone relative to the 1964±1970 annual average for the Northern Hemisphere (358N±908N), the Tropics (358N±358S), and the Southern Hemisphere (358S±908S). The Mount Pinatubo eruption occurred in June, 1991. Drawn from data of K. Tourpali, X. X. Tie, C. S. Zerofos, and G. Brasseur, J. Geophys. Res., 102, 23,955±23,962 (1997).

5.2.3.3 The Antarctic Ozone Hole

The foregoing trends in global stratospheric ozone, although statistically signi®cant, are admittedly small and obscured to a large extent by the seasonal variations that have been fairly regular for over 30 years. In striking contrast to this global behavior is the large depletion in total ozone above the Antarctic pole, ®rst reported in 1985.28 This depletion, called the Antarctic ozone hole, occurs in the Antarctic spring beginning in September and reaching a maximum (i.e., minimum total ozone) generally in early October. It disappears in November and early December as shifting springtime winds transport ozone-rich air from the middle and lower southern latitudes into the hole. The depletion of ozone since 1975 has been very dramatic: the average ozone concentration above the Antarctic in October declined from approximately 310 DU in 1975 to 170 DU in 1987, and a record low concentration of 91 DU was measured on October 12, 1993, followed by lows of 102 DU and 28

J. C. Farman, B. G. Gardner, and J. D. Shanklin, Large losses of total ozone in Antarctica reveal seasonal ClOx =NOx interaction, Nature, 315, 207±210 (1985).

118

5.2 REACTIONS IN THE UPPER ATMOSPHERE

98 DU during October of the 1994 and 1995 Antarctic winters, respectively; a low of 95 DU was observed for the 2000 Antarctic winter, occurring on October 1, 2000. Most of the change occurs in the lower stratosphere between about 10 and 24 km, a zone in which the ozone concentration has reached essentially zero during the October minimum since the record low year of 1993. The area covered by the hole has also continued to increase since ®rst observed in 1985; in 2000 it covered an area greater than 28  106 km2 , about the size of the North American continent and twice the size of Europe, extending to the tip of South America. Furthermore, after the hole breaks up, ozone-poor air drifts northward, resulting in increased ultraviolet radiation beyond Antarctica. It is now accepted that the polar vortex, which is the strong cyclonic ``whirlpool'' with winds upwards of 100 m=s circling the pole, virtually isolating the gases within it from the middle latitudes, and the extremely cold Antarctic night are the distinguishing factors that lead to the formation of the large zone of temporary ozone depletion. Temperatures in the swirling vortex can reach lower than 868C (187 K), which is the temperature at which ice particles can form, producing clouds even in very dry stratospheric air (probably on sulfate aerosols) at altitudes between 10 and 25 km. These clouds of ice crystals are called type II polar stratospheric clouds, or type II PSCs. In addition to these type II PSCs, however, clouds also form at higher temperaturesÐas high as 808C (193 K). These are called type I PSCs.29 Various possibilities have been suggested for the composition and phase or phases making up the type I clouds. These include crystals of nitric acid and water (particularly NAT, the nitric acid trihydrate HNO3 . 3H2 O) nucleated by frozen sulfate aerosols (sulfuric acid tetrahydrate, or SAT); ternary supercooled liquid solution droplets of water, nitric acid, and sulfuric acid; binary solutions of nitric acid and water; and a metastable water-rich nitric acid solid phase, as well as various combinations of these. The speci®c composition of type I PSCs may in fact be quite sensitive to the temperature and to the occurrence of freezing±thawing cycles during cloud formation. Most of the Antarctic ozone depletion occurs below 20 km. In this region there are virtually no oxygen atoms present for two reasons. First, the relatively high third-body pressure maximizes the pressure-dependent O ‡ O2 recombination, reaction (5-29); and second, the lack of sunlight during the Antarctic night minimizes the O-atom-producing photodissociation of O3 , reaction (5-30). As a result, neither mechanism (5-45) nor (5-46) can be occurring to any signi®cant extent. Nevertheless, observations clearly show that stratospheric chlorine species are involved in this dramatic ozone loss. The PSCs thus appear to be essential in formation of the Antarctic hole. 29

Type I PSCs are sometimes further broken down into types Ia and Ib.

119

5. ATMOSPHERIC PHOTOCHEMISTRY

It is now known that one of the key roles played by PSCs is to provide a surface on which ``active'' chlorine, such as ClO. , is converted to ``inactive'' chlorine by reactions such as ClO. ‡ NO2 ƒƒƒƒƒƒ! ClONO2 surface

…5-56†

Chlorine nitrate, ClONO2 , is called a ``reservoir'' species because it traps ``active'' chlorine in an ``inactive'' form. Another reservoir species is HCl, which can be formed by ``active'' chlorine atoms reacting with methane: Cl ‡ CH ! . CH ‡ HCl …5-57† 4

3

Neither of these reservoir molecules reacts with ozone, but the two do react together on PSC surfaces (a second key role for PSCs) by heterogeneous reactions such as surface

HCl ‡ ClONO2 ƒƒƒƒƒƒ! Cl2 ‡ HNO3

…5-58†

This reaction does not occur in the gas phase but is very fast on the ice surfaces and solutions making up the PSCs. Presumably an HCl molecule is adsorbed on the surface ®rst, followed by collision of a ClONO2 molecule and subsequent reactions represented by the overall reaction (5-58). Molecular chlorine, a ``storage'' molecule, accumulates and remains stored during the dark Antarctic night. When sunlight appears at the start of the Antarctic spring in September (beginning at the outer edge of the vortex and moving inward), molecular chlorine photodissociates into chlorine atoms hn

Cl2 ƒƒƒƒ! 2Cl

…5-59†

and initiates the following cycle that leads to the destruction of ozoneÐat rates sometimes greater that 1% per day: 2…Cl ‡ O3 ! ClO. ‡ O2 † M 2ClO. ƒƒƒƒ! ClOOCl …rate-determining step†

ClOOCl ƒƒƒƒ! ClO2 . ‡ Cl hn

ClO2 . ƒƒƒƒ! Cl ‡ O2 M

net:

hn; M

2O3 ƒƒƒƒƒƒ! 3O2

…5-60†

This mechanism can also be bromine-enhanced by mechanism (5-55). Other ``storage'' molecules are HOCl and ClNO2 ; they are produced by heterogeneous reactions like (5-58) and are also photolyzed in the Antarctic spring into Cl atoms, thereby further contributing to ozone destruction via (5-60).

120

5.2 REACTIONS IN THE UPPER ATMOSPHERE

For the observed large change in ozone concentrationÐthat is, essentially its complete destruction between 10 and 24 km above the Antarctic poleÐto occur by mechanism (5-60), the active ClO. concentration must remain relatively large for a month or so after the appearance of sunlight. Since ClO. is destroyed by (5-56), the concentration of NO2 needs to be kept low. This occurs through the heterogeneous formation of HNO3 , reaction (5-58), on the PSCs. On the other hand, evaporation of the PSCs in the sunlight and with rising temperatures will liberate HNO3 , which photodissociates at wavelengths less than 320 nm, freeing NO2 : hn … 320 nm†

HNO3 ƒƒƒƒƒƒƒƒƒ! . OH ‡ NO2

…5-61†

We see, then, that PSCs not only lead to the containment of ``storage'' molecules and the eventual release (in early spring) of ``active'' molecules that catalytically destroy ozone; they also can lead to release of species, such as NO2 , that destroy ``active'' molecules and thus prevent extensive ozone destruction. It turns out that when the temperatures remain low enough (i.e., below the condensation temperatures of the PSC phases present) long enough, the particles making up the PSCs grow and sedimentation occurs. This leads to permanent removal of HNO3 by transport to lower elevations, so that continued destruction of ozone occurs as a result of sustained high ClO. concentration. This process is called denitri®cation; it commences in the Antarctic during June and continues through the Antarctic winter and early spring. In addition to the PSCs, the sulfate droplets in the stratospheric aerosol layer (see Section 5.2.3.2) also provide surfaces for heterogeneous reactions that contribute to ozone depletion. For example, dinitrogen pentoxide, N2 O5 , reacts readily with water on sulfate aerosols to form nitric acid: sulfate aerosol

H2 O ‡ N2 O5 ƒƒƒƒƒƒƒƒƒƒƒ! 2HNO3

…5-62†

Since N2 O5 is formed from NO2 and NO3 , M

NO2 ‡ NO3 ƒƒƒƒ! N2 O5

…5-63†

the effect of reaction (5-62) is to tie up NO2 so that less of the ``inactive'' chlorine nitrate is formed by reaction (5-56), leaving more ``active'' ClO. available for the ozone-destroying cycles. The stratospheric sulfate aerosol layer during the Antarctic spring is below 20 km and has a broad maximum between 10 and 16 km. It is now believed that this sulfate layer was responsible for the 1993 record low Antarctic ozone hole. The slight moderations in the minimum depletions of 1994 and 1995 may be due to disappearance of aerosol from the Mount Pinatubo eruption after 1993, although the 1996 hole appeared earlier than usual (maximum ozone depletion on October 5) and was as intense as during the preceding several years.

5. ATMOSPHERIC PHOTOCHEMISTRY

121

Direct observations of stratospheric ClO. by aircraft ¯ying within the polar vortex conclusively show the involvement of CFCs and halons in the Antarctic ozone depletion process. For example, before the onset of the Antarctic spring and the development of the hole, the concentration of ClO. within the vortex from about 658S has been more than 100 times greater than outside the vortex at lower latitudes. When the hole has fully developed in late September and early October, there is complete correlation between the ozone depletion and ClO. enhancement as a function of latitude and altitude within the vortex. 5.2.3.4 Depletion of Ozone above the Arctic

For several reasons, the formation of an Arctic ozone hole is much less likely to occur than the Antarctic ozone hole (which we saw in the preceding section has been increasing in strength since 1985): The Arctic winters are generally warmer and rarely are cold enough for type II PSCs to form ( 868C): Warming toward the end of winter often occurs in February (equivalent to August in Antarctica) before there is enough sunlight to release active Cl and ClO. . The polar vortex usually is more distorted and breaks up by the end of March. In addition, during late winter and spring, ozone-rich air from the low latitudes above the equator is regularly transported northward at high altitudes to the North Pole region.30 This ``physical'' ozone increase will tend to obscure any chemically induced depletion of ozone. Nevertheless, as shown in Figure 5-8, total stratospheric ozone concentrations have in fact been signi®cantly decreasing in the Northern Hemisphere since 1988, and it is possible that an unusually cold and prolonged Arctic winter could lead to ozone depletion effects and to the development of an Arctic hole similar to that in the Antarctic. During the mid-1990s the Arctic winters had below average stratospheric temperatures. For example, the Arctic winter of 1995±1996 was the coldest ever observed up to that time, reaching a low of 888C on March 3 and producing a vortex roughly equivalent in size to that of the Antarctic in a typical winter. However, ®nal warming and breakup of the vortex began in early March, which was a month or two earlier than the usual Antarctic winter breakup. The Arctic winter of 1996± 1997 was also extremely cold, but it was unique in that the polar vortex did not form until late December. Nevertheless, the vortex developed fast after that and remained very strong and symmetrical, generally centered near the North 30

For example, this led, prior to 1988, to total late-spring ozone column concentrations greater than 450 DU above 708N latitudeÐmuch above the year-round global average of about 306 DU.

122

5.2 REACTIONS IN THE UPPER ATMOSPHERE

Pole, into late April, isolating the polar region from the inward ¯ow of ozonerich air. Anomalous low temperaturesÐbelow that needed for type I PSC formationÐcontinued through most of March. Concurrent high stratospheric concentrations of ClO. (as high as those in the Antarctic spring) in February indicated chemical ozone loss consistent with the halogen-catalyzed ozone depletion mechanism (5-60). The average Arctic ozone column concentration for the month of March (354 DU) was approximately 21% lower than pre1988 values and reached a record low of 219 DU on March 26, 1997. The Arctic winters of 1997±1998 and 1998±1999 were relatively warm, with low loss of ozone. However, the 1999±2000 Arctic winter was one of the coldest on record, with a low of 898C on January 10 and temperatures below that needed for type I PSC formation ( 808C) continuing over a longer period (from about November 20 to March 10) and a larger area than in any previously observed winter. Atmospheric measurements made from November, 1999 to April, 2000 showed greater ozone depletion in early February (approximately 1% a day) than in the cold 1995±1996 winter, leading to a clear ozone minimum over the Arctic pole that extended during February and March over an area comparable to a typical Antarctic hole. About 70% of the ozone near 19 km above the Arctic was depleted by the end of March. In addition, studies of oxides of nitrogen loss in the polar vortex from midJanuary to mid-March, 2000 (well after the breakup of the PSCs), showed the most severe Arctic denitri®cation ever observed. In contrast, during the 2000±2001 Arctic winter a strong polar vortex formed in October and November, but mild stratospheric warming occurred after that with temperatures rising above the PSC-forming threshold by midFebruary. This resulted in a heavy disturbance of the vortex and only a moderate total ozone loss for the season of approximately 20%. 5.2.3.5 Control of Ozone-Depleting Substances

Almost from the very beginning of the concern over potential stratospheric ozone depletion by nitrogen oxide or atomic chlorine from chloro¯uorocarbons there have been repeated callsÐmainly by the scienti®c communityÐfor reduction and eventual elimination of the industrial uses of CFCs. In 1978, almost all uses of CFCs for aerosols (primarily CFC-11) were banned in the United States. However, it was not until it was unequivocally shown by the Antarctic ozone hole that ozone could actually be destroyed in the stratosphere by human releases of chemicals into the troposphere that very strong action was of®cially taken by governments: the Montreal Protocol on Substances That Deplete the Ozone Layer, signed in 1988 and amended several times since then. By January 1, 2001, 175 countries had signed this agreement, which banned production of all halons (the major ®re-suppressant chemicals) as of January 1, 1994, and all CFCs, methyl chloroform (CH3 CCl3 ), and

5. ATMOSPHERIC PHOTOCHEMISTRY

123

carbon tetrachloride by January 1, 1996, for developed countries. The protocol has a 14-year grace period for developing countries (including production of small amounts by industrialized countries for use by developing countries), and also contains provisions allowing countries to petition for some exemptions based on lack of feasible chemical replacements, but it appears that relatively few such exemptions will be allowed. By 1993, the electronics industry in the United States had already almost completely stopped using CFCs (CFC-113) and methyl chloroform for precision cleaning, opting either for completely eliminating cleaning, or for cleaning with aqueous solutions. The United States capped consumption of methyl bromide (which accounts for about 10% of the ozone destruction) at 1991 levels in 1995, and a gradual phaseout started in 1999 with total consumption ban scheduled for 2005, in line with the 1997 amendments to the Montreal Protocol. The Japanese electronics industry phased out CFC use by 1995. There is some concern, however, about the possibilities for noncompliance with the provisions of the amended Montreal Protocol and with illegal trade of CFCs among developed and developing countries. Many of the compounds being developed and used for replacement of the CFCs are the hydrochloro¯uorocarbons, HCFCs, in which some of the CFC chlorine atoms have been replaced with hydrogen atoms that are readily abstracted by . OH radicals in the troposphere.31 As we saw Table 5-1, this greatly reduces their ozone depletion potentials, or ODPs.32 For example, HCFC-141b (CH3 CFCl2 Ðsee Table 3-2, note a, for determining compositions of CFCs, HCFCs, and HFCs from their names) has almost completely replaced CFC-11 as a blowing agent in the manufacture of polyisocyanurate foam insulation, and HCFC-124 (CHClFCF3 ) is an alternative for medical applications. However, since the HCFCs still contain one or more chlorine atoms, they still possess ®nite ODPs (see Table 5-1). As a result, the HCFCs also had production caps imposed by 1996 and phaseout of HCFC-141b in the United States and Europe by 2003 has been mandated. Replacement of all chlorine atoms with hydrogen atoms gives hydro¯uorocarbons, HFCs, that have zero ODP. The hydro¯uorocarbon HFC-134a (CH2 FCF3 ) is a replacement for CFC-12 in automobile air conditioners, and by the end of 1993 all new automobile air conditioners produced in the United States and Canada were using it. A planned replacement for CFC-11 as a polyurethane foam blowing agent is HFC-245fa (CF3 CH2 CHF2 ). HCFC-22 31 J. S. Francisco and M. M. Maricq, Atmospheric photochemistry of alternative hydrocarbons, in Advances in Photochemistry, vol. 20, D. C. Neckers, D. H. Volman, and G. von BuÈnau, eds., pp. 79±163. Wiley, New York, 1995. 32 The . CF3 radical, a fragment of HCFC-destroying reactions, is itself very stable and therefore potentially could also be involved in ozone-depleting catalytic cycles via CF3 O. and/or CF3 OO. radicals. However, laboratory studies and atmospheric models have shown that this is not the caseÐsee Section 8.6.2.2.

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5.2 REACTIONS IN THE UPPER ATMOSPHERE

(CHClF2 ), also a substitute for CFC-12, was widely used as a stationary air conditioner refrigerant, but it is being replaced by mixtures of various HFCs. Other compounds without chlorine that are being developed for CFC replacements are the ¯uorinated ethers, HFEs. For example, HFE-7100 (C4 F9 OCH3 )33 and HFE-7200 (C4 F9 OC2 H5 )34 are now being used commercially for applications employing liquids such as cleaning electronic equipment, secondary refrigerants, and carrier ¯uids for lubricants. HFE-7100 and HFE-7200 are trade names for isomeric mixtures of the materials; for example, HFE-7100 is a mixture of 40% of the normal isomer n-C4 F9 OCH3 , CF3 CF2 CF2 CF2 OCH3 , and 60% of the iso isomer i-C4 F9 OCH3 , …CF3 †2 CFCF2 OCH3 . They are readily oxidized in the troposphere by . OH radicals, giving short atmospheric lifetimes. The lifetime of 4.1 years given in Table 5-1 for HFE-7100 is a weighted average of 4.7 years for the normal isomer and 3.7 years for the iso isomer. Similarly, HFE-7200 has a lifetime of 0.8 years. Like the HFCs, they have zero ODPs. The ideal replacement chemicals might seem to be the fully ¯uorinated per¯uorocarbons (PFCs), since they are nontoxic and non¯ammable, and have zero ODPs. Since, however, they are very unreactive, with no known atmospheric sinks below the mesosphere, they have extremely long atmospheric lifetimesÐgreater than 50,000 years for CF4 (Table 5-1) and 10,000 years for C2 F6. Since in general they absorb radiation in the near-infrared ``window,'' they are very powerful greenhouse gases (see Sections 3.1.2 and 3.3.3). It is estimated, for example, that the impact of the PFCs on global warming may be greater than 5000 times than that of carbon dioxide 100 years after their release into the atmosphere. CFCs and HCFCs are also powerful greenhouse gases (i.e., large global warming potentials: see Table 3-2), although their atmospheric lifetimes (Table 5-1) are much less than those of the PFCs. Some HFCs such as HFC-23, a by-product in the production of HCFC-22, are also greenhouse gases. On the other hand, iodo¯uorocarbon compounds absorb strongly in the near-UV spectral region, leading to photodissociation (the CÐI bond is weaker than the CÐBr or CÐCl bond). Thus they have atmospheric lifetimes of only a few days and therefore have essentially zero ODPs and are not greenhouse gases. Tri¯uoromethyl iodide (CF3 I), which has an atmospheric lifetime of less than 2 days, is a promising replacement for H-1301 (CF3 Br) for controlling ®res, but its toxicity makes it unsuitable for use in enclosed spaces. 33 T. J. Wallington et al., Atmospheric chemistry of HFE-7100 (C4 F9 OCH3 ): Reaction with . OH radicals, UV spectra and kinetic data for C F OCH . and C F OCH O . radicals, and the 4 9 2 4 9 2 2 atmospheric fate of C4 F9 OCH2 O. radicals, J. Phys. Chem. A, 101, 8264±8274 (1997). 34 L. K. Christensen et al., Atmospheric chemistry of HFE-7200 (C4 F9 OC2 H5 ): Reaction with . OH radicals and fate of C F OCH O…
† and C F OCHO…
†CH radicals, J. Phys. Chem. A, 102, 4 9 2 4 9 3 4839±4845 (1998).

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5. ATMOSPHERIC PHOTOCHEMISTRY

For several decades prior to the discovery of the Antarctic ozone hole, the worldwide release of CFCs into the atmosphere exceeded a million tons per year. By 1993 this release of CFCs had dropped by 50%, and it is expected to dramatically decrease as the provisions of the revised and amended Montreal Protocol continue to be put into effect. As a result, the net chlorine and bromine concentrations in the troposphere peaked in 1994 and started to decline in 1995. Although tropospheric bromine continued to increase because of continuing release of halons, reactive stratospheric chlorine and bromine reached a maximum in 1999 or 2000. It is now calculated that if the provisions of the amended Montreal Protocol are adhered to, global stratospheric ozone should start to increase and the Antarctic ozone hole should start to shrink within 10 years, returning to 1979 levels by around the middle of the twenty®rst century.

5.2.4 Water in the Atmosphere We saw in Chapter 2 (Section 2.3.4) that the photolysis of water vapor is one of the two major sources of oxygen in our atmosphere. Reaction (2-1) represents the overall reaction leading to the formation of molecular oxygen and hydrogen. However, the precise mechanism of this reaction is not clear. The most likely path appears to be the photodissociation of water into H atoms, O atoms, and=or . OH radicals (depending on wavelength of light absorbed), followed by H ‡ . OH ! H2 ‡ O

…5-64†

and the three-body atom recombination reaction (5-21). Combination of two . OH radicals 2. OH ! H2 ‡ O2 …5-65† has also been proposed, however. Water absorbs radiation below 186 nm. The absorption spectrum consists of a continuum region (lmax ˆ 167:5 nm, s ˆ 5:2  10 18 cm2 =molecule), a banded region between about 122 and 143 nm superimposed on a second continuum (lmax ˆ 167:5 nm, s ˆ 9  10 18 cm2 =molecule), and a strongly banded region to below 100 nm corresponding to transitions of H2 O‡ . The presence of two continua indicates that two different excited states of H2 O are involved in the photochemistry of water. The major (99%) primary process between 186 and 140.5 nm is dissociation into ground-state hydrogen atoms and hydroxyl radicals, hn …186 140:5 nm†

H2 O ƒƒƒƒƒƒƒƒƒƒƒƒƒ! H ‡ . OH

…5-66†

126

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

providing a source of radicals for reactions (5-64) and (5-65). Dissociation of water into H2 and O may also be contributing in a minor way to absorption in this spectral region: H2 O ! H2 ‡ O …ground state or excited 1 D2 at  < 178 nm†

…5-67†

Between 140.5 and 124.5 nm the major reaction is still (5-66), but dissociations to excited OH* radicals hn …140:5 124:5 nm†

H2 O ƒƒƒƒƒƒƒƒƒƒƒƒƒ! H ‡ . OH

…5-68†

and to ground-state O atoms

hn …140:5 124:5 nm†

H2 O ƒƒƒƒƒƒƒƒƒƒƒƒƒ! 2H ‡ O

…5-69†

also occur. Below 124.5 nm (to 500 nm), minor products are excited H atoms and OH‡ ions in addition to the products from reactions (5-66), (5-67), (5-68), and (5-69). Since water does not absorb dissociating radiation above 186 nm, it will not be photodissociated in the troposphere, which is protected from the highenergy photons by oxygen and the stratospheric ozone layer. Photodissociation does occur in the mesosphere and in the upper stratosphere as a result of partial transmission through the UV window (Figure 5-7). Absorption of nondissociating infrared radiation by water in the troposphere is of course an important contributor to the greenhouse effect (Section 3.1.2). 5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG 5.3.1 The General Nature of Smog In polluted lower regions of the troposphere, particularly in urban environments (see Section 3.4), copious quantities of chemical compounds are released into the atmosphere, leading to a number of complex photochemical reactions producing a variety of eye and throat irritants, aerosols and reduced visibility, and other irritating or destructive species manifesting themselves in the general category of photochemical smog. Unlike the notorious smogs (smoke plus fog) that were a part of London life as well as that of many other highly industrial urban areas from the transition to coal in the thirteenth century until massive cleanup efforts were undertaken in the past few decades, photochemical smog is of fairly recent origin. It was ®rst detected through vegetation damage in Los Angeles in 1944 and is sometimes referred to as Los Angeles smog. However, it has now spread to virtually all major metropolitan areas and must be considered to be one of the most pressing actual or potential worldwide problems, with global aspects tran-

5. ATMOSPHERIC PHOTOCHEMISTRY

127

scending national boundaries. Also in contrast to the poisonous so-called London killer smogs,35 to date there do not appear to be major human disasters associated with photochemical smog. However, detailed epidemiological studies have shown that the concentrations of pollutantsÐparticularly of ozone but also materials such as particulate matter, the oxides of nitrogen, and volatile organic compounds (VOCs)Ðare suf®ciently high in photochemical smog to pose signi®cant threats to human health, particularly among the very young, the elderly, those suffering from chronic respiratory illnesses, and cigarette smokers. Common symptoms are sore throat, mild cough, headache, chest discomfort, decreased lung function, and eye irritation. Ozone also injures vegetation, leading to reduction of agricultural yield and biomass production. Potentially, photochemical smog can have serious long-range global effects on the earth's radiation balance through submicrometer aerosol formation, and global distribution that may cause unfavorable changes in weather patterns in addition to its in¯uence locally. Photochemical smog requires rather speci®c meteorological and geographical conditions to be produced in large quantities. For example, the photochemical reactions must occur in a stable air mass that traps the pollutants, which can result when there is a temperature inversion (Section 3.5). The Los Angeles Basin is particularly suited for this to occur, and in fact temperature inversions occur there about 80% of the time in hot summer months. Even though California has the strictest pollution control programs in the United States, this basin is still one of the worst in the country with respect to photochemical smog air pollutants.36 There are other signi®cant differences between ``London'' and ``Los Angeles'' smogs that suggest different remedial actions that might (or should) be taken in each case. London-type smogs occur mainly in the early morning hours in winter, where humidity is relatively high and virtually no solar photochemistry is taking place. Along with particulate matter, sulfur dioxide is the major contaminant, and this creates a chemically reducing atmosphere because of the ease of sulfur dioxide oxidation. On the other hand, photochemical smogs usually occur on warm sunny days (summer and winter) with initially clear skies and low humidity. Primary contaminantsÐthose that are emitted directly into the atmosphereÐare nitric oxide (NO), hydrocarbons, and carbon monoxide. Secondary contaminants, largely ozone and nitrogen dioxide, are produced by reactions of the primary contaminants in the atmosphere. They begin to build up during morning traf®c hours and reach peak 35 Over 3000 deaths were attributed to the four-day smog in London in December 1952; see Section 3.5. 36 Apparently Houston, Texas has joined Los Angeles as having the worst air quality in the United States (Houston air is focus of $20 million study, Chem. Eng. News, Nov. 6, 2000, pp. 32±33).

128

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

intensity in midday, although hourly variations occur depending on automobile traf®c=time distributions and even time variations for different constituents (Figure 5-9). Natural and nonnatural sources of volatile organic compounds (VOCs) and oxides of nitrogen are covered in detail in Section 6.7. Naturally released methane and carbon monoxide can lead to photochemically induced ozone generation and formation of a variety of oxygen- and nitrogen-containing compounds if the nitrogen oxides concentration is suf®ciently high. These reactions will be covered in the next section. The importance of the anthropogenic sources is that in an urban environment, with the appropriate climatic, geographic, and solar radiation conditions, they generate suf®ciently high concentrations of the pollutants to undergo drastically more complex photochemical and secondary reactions, leading to photochemical smog. Hundreds of individual species are continuously dischargedÐat rates and light intensities that vary depending on the time of day and so onÐinto a complex moving air mass of variable size in which thousands of simultaneous and consecutive reactions take place. Complete quantitative mathematical modeling of photochemical smog requires reliable primary emission rates over a period of time and ambient concentrations of VOCs, physical three-dimensional

0.16

NO2

Concentration (ppm)

0.12 O3 NO

0.08

0.04

0 12

2

4

6 AM

8

10

12

2

4

6 PM

8

10

12

Hour of day FIGURE 5-9 Photochemical smog buildup in Los Angeles, California, on July 10, 1965. Redrawn from K. J. Demerjian, J. A. Kerr, and J. G. Calvert, Adv. Environ. Sci. Technol., 4, 1 (1974).

129

5. ATMOSPHERIC PHOTOCHEMISTRY

gas-phase (plume) transport behavior that includes topography, and accurate reaction rate data for the many hundreds of individual chemical processes taking place. Reasonable computer simulations generally lump the hundreds of individual VOC contaminants into a manageable smaller number of groups or classes of chemical species with similar structure and reactivity, such as alkenes or aldehydes. Each group is then represented by ``surrogate'' species.37 In Section 5.3.3 we consider several reactions that are well established as primary steps in photochemical smog initiation in the presence of VOCs and associated generation of the accompanying obnoxious products.

5.3.2 Nitrogen Oxides (NOx ) in the Absence of Volatile Organic Compounds (VOCs) As pointed out in Section 6.7, the main anthropogenic sources of nitrogen oxides in a polluted atmosphere are mobile and stationary petroleum and coal combustion chambers, where inside temperatures and pressures are high enough for the ®xation of nitrogen to occur, N2 ‡ xO2 ! 2NOx

…5-70†

(NOx represents a mixture of oxides of nitrogenÐmainly NO and NO2 ) and where quenching to low temperatures outside the chambers is rapid enough to prevent the thermodynamically favored back-reaction (dissociation) from occurring. The major oxide of nitrogen produced is nitric oxide, NO, a relatively nontoxic gas, along with some nitrogen dioxide, NO2 . The concentration of NO in a polluted atmosphere is quite sensitive to automobile traf®c patterns, in general being a maximum during the peak morning traf®c hours (Figure 5-9). However, NO does not absorb radiation above 230 nm, and therefore it cannot be the primary initiator of photochemical reactions in a polluted lower atmosphere. On the other hand, NO2 is a brown gas with a broad, intense absorption band absorbing over most of the visible and ultraviolet regions with a maximum at 400 nm (smax  6  10 19 cm2 =molecule) as shown in Figure 5-10, and this gas is a major atmospheric absorber leading to photochemical smog. As we shall see later, there are other light-absorbing species present at very low concentrations in a polluted atmosphere that can also initiate the complex photochemical reactions. 37

A mathematical modeling [R. A. Harley, A. G. Russell, and G. R. Cass, Mathematical modeling of the concentrations of volatile organic compounds: Model performance using a lumped chemical mechanism, Environ. Sci. Technol., 27, 1638±1649 (1993)] based on the Southern California Air Quality Study of the Los Angeles Basin on August 27±29, 1987 involved 35 species and 106 chemical reactions, with the atmospheric diffusion equation solved for each of the chemical species.

130

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

7

(10–19cm2/molecule)

6 5 4 3 2 1 0 300

350

400

450 Wavelength (nm)

500

550

600

FIGURE 5-10 Absorption spectrum of NO2 at room temperature averaged over 5-nm intervals. Drawn from data of M. H. Harwood and R. L. Jones, J. Geophys. Res., 99, 22,955±22,964 (1994).

The dissociation energy of NO2 is 3.12 eV, which corresponds to a photon having a wavelength of 397.5 nm, and absorption below this wavelength leads to almost complete photodissociation (f  1)38: hn …< 397:5 nm†

NO2 ƒƒƒƒƒƒƒƒƒƒƒ! NO ‡ O

…5-71†

In the absence of other species, molecular oxygen may be formed by a reaction of an O atom with NO2 , reaction (5-43), and indeed the quantum yield of O2 formation approaches unity below 380 nm. In the presence of ground-state molecular oxygen, however,
ozone is produced by the three-body reaction (5-29) between O2 and O 3 P2 . Combination of reactions (5-71), (5-29), and (5-42) leads to the photostationary state NO2 ‡ O2

hn …NO2 †; M

…5-72† ƒƒ ƒƒƒƒƒƒ! O3 ‡ NO   and hence to a steady-state ozone concentration, O3 SS . Since NO and NO2 appear on different sides of reaction (5-72), the ozone concentration   will depend on the ratio of nitrogen oxide concentrations: that is, O3 ss is 38

Some dissociation even occurs at wavelengths greater than 397.5 nmÐfor example, the O2 quantum yield is 0.36 at 404.7 nmÐand thus energetically below the dissociation energy. But this dissociation is strongly temperature dependent and presumably is due to the contributions of internal rotational and vibrational energies.

131

5. ATMOSPHERIC PHOTOCHEMISTRY

    proportional to  NO  2 = NO . However, since we have assumed a photostationary state, O3 SS will be a function of the light intensity. Thus, NO2 is the primary light-absorbing species in the atmosphere leading to photochemical smog and the ozone concentration is enhanced by increasing NO2 , but NO is the major oxide of nitrogen produced in hightemperature combustion chambers. Since the small amount of NO2 produced directly would be completely depleted in a very short time in direct sunlight, at least one additional process leading to the oxidation of NO to NO2 is required to produce the quantities of O3 and other products generated in a polluted atmosphere. It is now agreed that the hydroxyl (. OH) and hydroperoxyl (HO2 . ) radicals play key roles in the rapid oxidation of NO to NO2 in the absence of VOCs.39 The HO2 . radical is directly involved: NO ‡ HO . ! NO ‡ . OH …5-73† 2

2

However, we will see shortly that HO2 . radicals are formed in free-radical chain mechanisms in which . OH radicals serve as chain carriers, so that . OH and HO2 . are interconverted provided suf®cient NO is present for reaction (5-73) to be dominant. The major source of . OH in the troposphere is the reaction
1 primary  of excited O D2 atoms with water, reaction (5-35), following photolysis of ozone below 310 nm [see reaction (5-32)]. The global-averaged noontime concentration of the hydroxyl radical in the lower troposphere is very lowÐof the order of 106 molecules/cm3 Ðwith a lifetime of approximately one second. It does not react with the major tropospheric constituents (N2 , O2 , CO2 , H2 O), but it is the major initiator of oxidation in photochemical smog generation and in the removal of most trace gases in the atmosphere. The HO2 . radical can react with ozone, regenerating the . OH radical HO . ‡ O ! . OH ‡ 2O …5-74† 2

3

2

It can also self-combine to form hydrogen peroxide 2HO . ! H O ‡ O 2

2

2

2

…5-75†

which dissolves in fog and clouds and is washed out of the troposphere by rain. In the absence of VOCs, two species with major natural and anthropogenic sources that lead to HO2 . (hence to oxidation of NO to NO2 ) are carbon

39 Thermal oxidation of NO to NO2 by O2 is thermodynamically feasible but is not signi®cant at normal NO pressures in the atmosphere. Similarly, the oxidation of NO by ground-state O atoms is unimportant at the low O-atom concentrations in the lower troposphere.

132

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

monoxide, CO, and methane, CH4 (see Section 2.2). Carbon monoxide reacts rapidly (with very low activation energy) with the hydroxyl radical CO ‡ . OH ! CO2 ‡ H;

k298  2  10

13

cm3 molecule

1

s

1

…5-76†

followed by the very fast three-body (essentially triple-collision frequencyÐsee Section 4.3) combination reaction H ‡ O2 ƒƒƒƒ! HO2 . M

…5-77†

Coupling these two reactions with reaction (5-73) gives the CO chain mechanism, with . OH the primary chain carrier and HO2 the secondary chain carrier: CO ‡ . OH ! CO2 ‡ H M H ‡ O2 ƒƒƒƒ! HO2 . NO ‡ HO . ! NO ‡ . OH 2

2

. OH; M net: CO ‡ NO ‡ O2 ƒƒƒƒƒƒ! CO2 ‡ NO2

…5-78†

However, this CO chain does not contribute to the overall NO oxidation to the extent that methane does in a similar chain. The . OH radical is the major tropospheric ``sink'' for methane via the reaction . OH ‡ CH ! . CH ‡ H O …5-79† 4

3

2

Reaction (5-79) results in a tropospheric lifetime for methane of about 12 years. The major fate of the methyl (. CH3 ) radical in the troposphere is the very fast (also of the order of a triple collision) three-body combination reaction with O2 to form CH3 O2 . 40: M . CH ‡ O ƒƒƒ …5-80† ƒ! CH3 O2 . 3 2 The methylperoxy radical, CH O . , can react in the troposphere with a variety 3

2

of species. 1. If the NO concentration is high enough, NO is oxidized to NO2 in a fast reaction analogous to reaction (5-73), producing the methoxy (CH3 O. ) radical CH O . ‡ NO ! CH O. ‡ NO …5-81† 3

2

3

2

Actually, under tropospheric conditions the concentrations of . CH3 and O2 and the lifetime of CH3 O2 . are such that the reaction order varies between 2 and 3 depending on the overall pressure. That is, at very low pressures the reaction order approaches 3, whereas at high pressures it approaches 2. 40

133

5. ATMOSPHERIC PHOTOCHEMISTRY

followed by CH3 O. ‡ O2 ! H2 CO ‡ HO2 .

…5-82† . The OH radical is regenerated by reaction (5-73). Combination of these reactions gives the . OH-initiated methane chain reaction for oxidation of NO: . OH ‡ CH ! . CH ‡ H O 4

. CH

3

2

‡ O2 ƒƒƒƒ! CH3 O2 . CH3 O2 . ‡ NO ! CH3 O. ‡ NO2 CH O. ‡ O ! H CO ‡ HO . M

3

3

2

2

2

HO2 . ‡ NO ! NO2 ‡ . OH net:

. OH; M CH4 ‡ 2O2 ‡ 2NO ƒƒƒƒƒƒƒƒ! H2 CO ‡ 2NO2 ‡ H2 O

…5-83†

[Reaction (5-75) is a possible chain-terminating step in this mechanism.] This gives an increase in ozone by the photostationary state (5-72). 2. On the other hand, if the tropospheric NO concentration is low (as in some very clean, unpolluted areas), instead of reacting with NO, the methylperoxy radical CH3 O2 . reacts with HO2 . , forming methyl hydroperoxide: CH O . ‡ HO . ! CH O H ‡ O …5-84† 3

2

2

3

2

2

In effect reaction (5-84) serves as a ``sink'' for both . OH and HO2 . , since the methane chain reaction (5-83) is now terminated and the interconversion of . OH and HO . is restricted, and this leads to a net decrease in ozone. The 2 methylperoxy radical also rapidly combines with NO2 in the three-body reaction CH3 O2 . ‡ NO2 ƒƒƒƒ! CH3 O2 NO2 M

…5-85†

but this reaction is generally not important in the troposphere because of the fast decomposition of methylperoxynitrate (CH3 O2 NO2 ) back to the reactants. Formaldehyde, H2 CO, is an overall product of the methane chain reaction (5-83), formed in the chain by the reaction of the methoxy radical with molecular oxygen (step 4).41 It absorbs weakly in the near-ultraviolet spectral 41

Formaldehyde is also a primary emission product of hydrocarbon combustion, and is produced in the photooxidation of a wide variety of higher hydrocarbons in VOC-containing atmospheres (next section); its average concentration in urban areas is approximately 3±16 parts per billion by volume (ppbv).

134

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

region. Its gas-phase absorption spectrum is strongly banded, with
lmax 305 nm s305  7  10 20 cm2 =molecule , and only very weak absorption near the visible region (e.g., s370  2  10 21 cm2 /molecule). This  absorption forms an excited formaldehyde . molecule, H2 CO , which dissociates either to H and the formyl radical HC O, . hn H2 CO ƒƒƒƒ! H ‡ HC O …5-86† or to H2 and CO:

hn

H2 CO ƒƒƒƒ! H2 ‡ CO

…5-87†

Reaction (5-86) dominates below roughly 330 nm, corresponding to the dissociation energy of H2 CO, while (5-87) is the major dissociation above 330 nm. Thus, H2 CO is a source of HO2 . radicals by reaction (5-77) and by . …5-88† HC O ‡ O2 ! HO2 . ‡ CO . Formaldehyde also reacts with OH . OH ‡ H CO ! H O ‡ HC. O 2 2 . and combines with HO2 to form initially an alkoxy radical HO . ‡ H CO ! HO CH O. 2

2

2

2

…5-89†

…5-90†

which rapidly isomerizes to a peroxy radical HO2 CH2 O. ! . O2 CH2 OH

…5-91†

However, excitation and subsequent dissociation steps, reactions (5-86) and (5-87), dominate in an atmosphere free from VOCs, leading to a noonday overall atmospheric lifetime of approximately 3 hours for formaldehyde. A reaction not yet considered is the reaction between NO2 and O3 : NO2 ‡ O3 ! NO3 . ‡ O2

…5-92†

The nitrate radical (NO3 . ) plays an important role in photochemical smog, particularly in nighttime reactions involving aldehydes and simple ole®ns. It reacts at close to collisional frequency with NO to produce NO2 : NO3 . ‡ NO ! 2NO2

…5-93†

It combines with NO2 to form dinitrogen pentoxide, N2 O5 , by the reversible reaction NO3 . ‡ NO2

M

! N2 O5

…5-94†

135

5. ATMOSPHERIC PHOTOCHEMISTRY

with a formation constant K298 ˆ 4:5  10 11 cm3 =molecule. (Equilibrium is reached in about one minute under tropospheric conditions.) N2 O5 also reacts with water to form nitric acid, N2 O5 ‡ H2 O ! 2HNO3 …5-95† . . thus providing a sink for both NO3 and NO2 . In the daytime NO3 is rapidly photolyzed to NO and O2 NO3 . ƒƒƒƒ! NO ‡ O2

…5-96†

NO3 . ƒƒƒƒ! NO2 ‡ O

…5-97†

hn

or to NO2 and O

hn

so that its daytime concentration is very low. However, at night it may be one of the most important tropospheric oxidizing agents. Additional reactions of NO3 . in the presence of methane and VOCs are covered next.

5.3.3 Reactions in Urban Atmospheres Containing Volatile Organic Compounds We have just seen that the ozone concentration can be enhanced even in a VOC-free atmosphere containing oxides of nitrogen and methaneÐanthropogenic and=or naturalÐor, to a lesser extent, carbon monoxide. These ozoneproducing processes are generally well understood now, and they give reasonable simulations in tropospheric computer modeling. In polluted urban areas, however, chemical reactions of VOCs dominate over those involving methane, leading to considerably more complexity because of the number (hundreds) of VOCs and their diverse chemistry. An excellent review by Atkinson42 covers reactions under tropospheric conditions of several classes of organic compounds, such as hydrocarbons (alkanes, alkenes, alkynes, and aromatics and substituted aromatics) and oxygen- and nitrogen-containing compounds, and their degradation products. Although complete coverage of the photochemical smog mechanism is beyond the scope of this book, this section summarizes some of the more important types of these reactions. One of the major tools used in determining the individual chemical processes taking place is the environmental chamber.43 Also called smog cham42 R. Atkinson, Gas-phase tropospheric chemistry of organic compounds, Monograph no. 2 of The Journal of Physical and Chemical Reference Data, J. W. Gallagher, ed. American Chemical Society and the American Institute of Physics for the National Institute of Standards and Technology, Gaithersburg, MD, 1994. 43 A coverage in depth of environmental chambers is given in B. J. Finlayson-Pitts and J. N. Pitts Jr., Chemistry of the Upper and Lower Atmosphere: Theory, Experiments, and Applications, Academic Press, San Diego, CA, 2000.

136

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

bers, these vessels are often large (from tens to hundreds of cubic meters) receptacles in which reactant mixtures close to actual atmospheric conditions of concentration, pressure, relative humidity and temperature are illuminated with solar spectral distribution light. A typical smog chamber experiment for a mixture of NO, NO2 , and hydrocarbon (propene, C3 H6 ) is shown in Figure 5-11. It is seen that the photostationary state projected for a VOC-free atmosphere [equation (5-72)] is destroyed by addition of the hydrocarbon. NO is rapidly oxidized to NO2 , O3 is produced after an induction period, and the propene is oxidized to CO, CO2 , and a variety of oxygen- and nitrogencontaining organic compounds. This reaction mixture is of course an extreme simpli®cation, containing only one hydrocarbon instead of the hundreds of VOC species emitted into a polluted urban environment. Note, however, that it qualitatively agrees with the actual photochemical smog buildup shown in Figure 5-9. That is, NO is rapidly oxidized to NO2 in the presence of organic compounds (the VOCs emitted along with NO into the atmosphere starting around 6 a .m . from automobile exhausts) and the ozone builds up only after an induction period, during which the concentration of NO is lowered until O3 is no longer destroyed by reaction (5-42).

2.0

Concentration (ppm)

C3H6 CO

1.5

1.0 NO

NO2

CH3CHO O3

0.5

PAN

60

120

180 240 Irradiation time (min)

300

360

FIGURE 5-11 Typical photochemical smog chamber results for a mixture of hydrocarbon, NO, and air. Drawn from data of A. P. Altshuller, S. L. Kopczynski, W. A. Lonneman, T. L. Baker, and R. L. Slater, Environ. Sci. Technol., 1, 899 (1967); and K. J. Demergian, J. A. Kerr, and J. G. Calvert, The Mechanism of Photochemical Smog Formation, in Advances in Environmental Science and Technology, J. N. Pitts Jr., and R. L. Metcalf, eds., 4, p. 1. Wiley, New York, 1974.

137

5. ATMOSPHERIC PHOTOCHEMISTRY

As we will see in this section, the organic alkyl (R. ), alkoxy (RO. ), and alkylperoxy (RO2 . ) radicals (in addition to . OH and HO2 . ) are important intermediates in the tropospheric degradation of VOCs and the formation of photochemical smog. Each is involved in many chain-propagating steps in which NO is converted to NO2 before being terminated by reactions such as (5-75) or (5-103), shown later. We have seen that the methyl (. CH3 ) radical is produced in the chain-initiating H-atom abstraction by the . OH radical [reaction (5-79)] in the methane chain; similarly, this is the major mode of formation of alkyl and substituted alkyl radicals from several classes of compounds: . OH ‡ RH ! R. ‡ H O 2

…5-98†

With alkenes, however, the major reaction of OH is addition to the carbon± carbon double bond to give b-hydroxyalkyl radicals, . M RHC ˆ CHR0 ‡ . OH ƒƒƒƒ! RHC C…OH†HR0

…5-99†

with only a small fraction of the . OH radicals involved in H-atom abstraction. Radicals are also produced by photolysis of some VOCs. In Section 5.3.2, for example, we saw . that the photolysis of formaldehyde below 330 nm generates H and HC O radicals [reaction (5-86)]. In a similar manner, higher aldehydes such as acetaldehyde, propanal, or butanal, which are formed in the tropospheric degradation of many VOCs, photodissociate into an R. radical and the formyl radical: . hn RCHO ƒƒƒƒ! R. ‡ HC O …5-100†

Smog chamber studies of hydrocarbon±NO mixtures have shown that addition of aldehydes does indeed enhance NO oxidation and production of secondary pollutants. Most of the alkyl and substituted alkyl radicals very rapidly combine with O2 to produce alkylperoxy radicals: M R. ‡ O2 ƒƒƒƒ! RO2 .

…5-101†

For allyl, benzyl, substituted benzyl, or alkyls with more carbons than ethyl, reaction (5-101) is second order under atmospheric conditions (see footnote 40). The b-hydroxyalkyl radicals formed by the addition of . OH to the alkene double bond [reaction (5-99)] . also rapidly add to O2 forming b-hydroxyalkylperoxy radicals, RHC…O 2 †C…OH†HR0 . All the alkylperoxy (RO2 . ) radicals react with NO with approximately the same rate constant. Both CH3 O2 . and C2 H5 O2 . primarily oxidize NO to NO2 , forming an alkoxy radical: RO2 . ‡ NO ! RO. ‡ NO2

…5-102†

138

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

However, for the larger alkylperoxy radicals, addition to form organic nitrates also occurs, RO2 . ‡ NO ƒƒƒƒ! RONO2 M

…5-103†

with reaction (5-103) becoming more important with increasing number of carbon atoms in R. We thus see that the HO2 . and RO2 . radicals generated in an oxygen environment by the . OH radical in the degradation of many VOCs are at least qualitatively the major contributors to the enhanced NO-to-NO2 oxidationÐand therefore to buildup of O3 Ðin photochemical smog via reactions like (5-102) and chain reactions similar to the methane chain, (5-83). Other radicals generated from VOCs react differently with O2 other than by the addition . reaction (5-101). For example, we saw in reaction (5-88) that the formyl (HC O) radical from the photolysis of formaldehyde reacts with O2 to give HO2 . and CO. The a-hydroxy radicals also react with O2 via H-atom abstraction to give the HO2 . radical, as for example the simplest a-hydroxy radical, . CH2 OH: . CH OH ‡ O ! HO . ‡ H CO …5-104† 2 2 2 2 This is the only process leading to the loss of . CH2 OH under atmospheric conditions. The vinyl radical . C2 H3 initially adds to O2 across the. double bond to form a C2 H3 O2 adduct, which decomposes to H2 CO and HC O giving the overall reaction . . HC ˆ CH2 ‡ O2 ! H2 CO ‡ HC O …5-105† . The three major reactions of the alkoxy or substituted alkoxy (RO ) radical from (5-102) in the troposphere are reaction with O2 , unimolecular decomposition, and (for four or more carbon atoms) unimolecular isomerization. However, all these reactions eventually lead to formation of HO2 . and=or the oxidation of NO to NO2 by reactions similar to (5-102).44 Aliphatic aldehydes and ketones are products of the atmospheric degradation of a wide variety of VOCs, primarily from reactions of alkoxy and alkylperoxy radicals. The . OH radical reacts with carbonyl compounds via H-atom abstraction; with the aldehydes, abstraction is mostly from the primary carbon to give the acyl radical and water: . OH ‡ RCHO ! RC. O ‡ H O …5-106† 2 Acyl radicals are also produced by H-atom abstraction from aldehydes by the NO3 . radical, giving HNO3 , and by other organic radicals, R0 . : 44 For example, with the smallest alkoxy radical, methoxy …H3 CO. †, H3 CO. ‡ O2 ! H2 CO ‡ HO2 . .

139

5. ATMOSPHERIC PHOTOCHEMISTRY

. R . ‡ RCHO ! R0 H ‡ RC O

…5-107†

Acyl radicals combine with O2 to form peroxyacyl radicals RC…O†O2 . . M RC O ‡ O2 ƒƒƒƒ! RC…O†O2 .

…5-108†

which further contributes to NO oxidation, hence to photochemical smog, by the rapid reaction RC…O†O . ‡ NO ! RC…O†O. ‡ NO …5-109† 2

2

followed by formation of another alkylperoxyl radical from the RC…O†O. (acyloxy) radical: RC…O†O. ‡ O2 ! RO2 . ‡ CO2 …5-110† The peroxyacyl radical also combines with NO2 in a three-body reaction to produce peroxyacyl nitrate, RC…O†OONO2 : RC…O†O2 . ‡ NO2

M

! RC…O†OONO2

…5-111†

The simplest and most abundant peroxyacyl nitrate is peroxyacetyl nitrate (PAN), CH3 C…O†OONO2 . PAN is an important component of photochemical smog. For example, it is highly phytotoxic: one of the most toxic compounds known for vegetation. It is also a potent lachrymator, and is perhaps the major eye irritant in photochemical smog. It is also a greenhouse gas in that it absorbs radiation in the tropospheric IR ``window.'' It is unstable, decomposing thermally by the reverse of reaction (5-111) to the peroxyacetyl radical and NO2 ; yet it is suf®ciently stable in the absence of NO to aid in the transport of nitrogen oxides to initially unpolluted ``downwind'' areas. In fact, it has been detected even in remote parts of the troposphere. The next most abundant peroxyacyl nitrate is peroxypropionyl nitrate (PPN), C2 H5 C…O†OONO2 ; although it may be more phytotoxic, its concentration is only about 10±20% that of PAN. In addition to its key role in the NO-to-NO2 oxidation, the hydroxyl radical is also the primary oxidant and remover of VOCs and other pollutants in the atmosphere. Brie¯y, its major reactions with VOCs, in addition to those already given are addition, across the carbon±carbon triple bond in alkynes and to the aromatic ring in monocyclic aromatics and in naphthalene and methyl- and dimethyl-substituted naphthalenes, and H-atom abstraction, from ethers, a, b-unsaturated carbonyls, and alkyl nitrates, and from both the CÐH and OÐH bonds in alcohols. The hydroxyl radical can also initiate the oxidation of reduced forms of sulfur such as hydrogen sul®de to . SH radicals: . OH ‡ H S ! H O ‡ . SH 2 2

…5-112†

140

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

Further oxidation of . SH leads to sulfur dioxide, SO2 . The hydroxyl radical is also involved in the continuing oxidation of SO2 by the addition reaction to form the HOSO2 . radical, reaction (5-52), followed by oxidation to sulfuric acid, H2 SO4 , and sulfate aerosol droplets in the presence of water.45 Large amounts of sulfur oxides are released into the troposphere over industrialized areas, and they become the major acidic component of acid rain (see Section 11.4). While ozone is the major contaminant product and its concentration is taken as the measure of the intensity of photochemical smog, it also contributes to decomposition reaction of the VOCs. For example, the addition of O3 to the double bond in alkenes is a major pathway in their atmospheric decomposition. An energy-rich ozonide is formed, which rapidly decomposes by breaking the CÐC single bond and either of the two OÐO single bonds to . form a carbonyl and a biradical RR C OO. . This energy-rich biradical either decomposes, forming a variety of products including the . OH radical, or reacts with aldehydes, H2 O, NO2 , and so on. We have seen that the nitrate radical is formed by the reaction of NO2 with ozone (5-92), that it is in equilibrium with NO2 and N2 O5 (5-94), that it reacts with NO to produce NO2 (5-93), and that it is photolyzed to NO ‡ O2 (5-96) or to NO2 ‡ O (5-97). It also reacts with alkanes via H-atom abstraction, similar to . OH reactions: NO . ‡ RH ! R. ‡ HNO …5-113† 3

3

However, although the NO3 . concentration is greater at night than during the day because of its daytime photolysis, it is nevertheless much less important at nighttime than the . OH radical is during the daytime as a source of alkane decomposition. NO3 . readily reacts with alkenes by addition to the carbon± carbon double bond, followed by rapid addition to O2 . The resulting bnitratoalkylperoxy radicals can react with HO2 . and RO2 . radicals, and can also reversibly add NO2 to give the unstable nitratoperoxynitrates, which may serve as temporary ``sinks'' for the peroxy radicals.

5.3.4 Summary of Photochemical Smog Only a very small portion of the hundreds of reactions possible in polluted atmospheres have been presented, but these are representative of the types of mechanism being considered to account for photoinitiation, oxidation of NO and VOCs, and formation of noxious products associated with photochemical smog. Figure 5-12 shows a computer integration of the differential kinetic rate 45 The oxidation of HOSO2 . to H2 SO4 in the troposphere is not simply the addition of another . OH radical. Rather, it is mostly by heterogeneous reactions taking place in cloud droplets, probably involving hydrogen peroxide, H2 O2 .

141

5. ATMOSPHERIC PHOTOCHEMISTRY

0.30

Concentration (ppm)

0.25

0.20 O3

0.15 RCHO

0.10

PAN

NO2 HNO3

0.05 RH

NO

HCHO

H2O2

0 0

50

100

150 Time (min)

200

250

300

FIGURE 5-12 Computer simulation of a generalized mechanism representing photochemical smog (see text). Redrawn from J. H. Seinfeld and S. N. Pandis, Atmospheric Chemistry and Physics: From Air Pollution to Climate Change. Copyright # 1998. New York: John Wiley & Sons, Inc. Used by permission of John Wiley & Sons, Inc.

equations representing a generalized mechanism involving 20 stepsÐincluding many of the reactions and organic species given earlierÐfor a system initially containing equal concentrations (0.10 ppmv) of NO, H2 CO, and organic species groups RH (alkanes) and RCHO (aldehydes), and a small amount (0.01 ppmv) of NO2 .46 Compare this computer simulation with the photochemical smog chamber results (that however did not have initial amounts of H2 CO and RCHO), where RH ˆ C3 H6 , shown in Figure 5-11. Note the qualitative similarities between the two: the rapid conversion of NO to NO2 and the subsequent loss of NO2 ; the slower loss of RH (C3 H6 in Figure 5-11) and buildup of ozone, after most of the NO has reacted; the buildup and decay of RCHO (CH3 CHO in Figure 5-11); and the induction period in the 46 J. H. Seinfeld and S. N. Pandis, Atmospheric Chemistry and Physics: From Air Pollution to Climate Change, pp. 292±298. Wiley, New York, 1998.

142

5.3 PHOTOPROCESSES IN THE TROPOSPHERE: PHOTOCHEMICAL SMOG

production of PAN. Applicable trends are also evident on the measurements of actual atmospheric conditions (Figure 5-9). Although so far there have not been any large disasters directly attributable to photochemical smog, the quality of the environment is seriously degraded by its presence, and it is now widespread in the industrial world. Ambient ozone is one of the most pervasive environmental problems facing urban and regional areas. In the next chapter we review many of the remedies and legislative actions being undertaken to reduce the emissions of particulates, VOCs, carbon monoxide, and oxides of nitrogen (primarily from automobiles), and to suppress or limit secondary pollutants. There continues to be a great need for reliable kinetic data for the many chemical processes occurring in a polluted environment and for accurate models to simulate their physical and chemical behaviors. Additional Reading Atkinson, R., Gas-phase tropospheric chemistry of organic compounds, Monograph no. 2 of The Journal of Physical and Chemical Reference Data, J. W. Gallagher, ed. American Chemical Society and the American Institute of Physics for the National Institute of Standards and Technology, Gaithersburg, MD, 1994. Barker, J. R., ed., Progress and Problems in Atmospheric Chemistry. World Scienti®c, Singapore, 1995. Biggs, R. H., and M. E. B. Joyner, eds., Stratospheric Ozone Depletion=UV-B Radiation in the Biosphere. Springer-Verlag, Berlin, 1994. Birks, J. W., J. G. Calvert, and R. E. Sievers, eds., The Chemistry of the Atmosphere: Its Impact on Global Change: Perspectives and Recommendations. American Chemical Society, Washington, DC, 1993. Brasseur, G. M., J. J. Orlando, and G. S. Tyndall, eds., Atmospheric Chemistry and Global Change. Oxford University Press, Oxford, U.K., 1999. Brimblecombe, P., Air Composition and Chemistry, 2nd ed. Cambridge University Press, Cambridge, U.K., 1996. Calvert, J. G., ed., The Chemistry of the Atmosphere: Its Impact on Global Change. Blackwell Scienti®c Publications, Oxford, U.K., 1994. Finlayson-Pitts, B. J., and J. N. Pitts Jr., Chemistry of the Upper and Lower Atmosphere: Theory, Experiments, and Applications. Academic Press, San Diego, CA, 2000. Kondratyev, K. Ya., and C. A. Varotsos, Atmospheric Ozone Variability: Implications for Climate Change, Human Health, and Ecosystems. Praxis Publishing, Chichester, U.K., 2000. Makhijani, A., and K. R. Gurney, Mending the Ozone Hole. Science, Technology, and Policy. MIT Press, Cambridge, MA, 1995. Moortgat, G. K., A. J. Barnes, G. LeBras, and J. R. Sodeau, eds., Low-Temperature Chemistry of the Atmosphere. Springer-Verlag, Berlin, 1994. Newton, D. E., The Ozone Dilemma: A Reference Manual. ABC-CLIO, Santa Barbara, CA, 1995. Seinfeld, J. H., Rethinking the Ozone Problem in Urban and Regional Air Pollution, Report of the Committee on Tropospheric Ozone Formation and Measurement, J. H. Seinfeld, Chairman. National Academy Press, Washington, DC, 1991. Seinfeld, J. H., and S. N. Pandis, Atmospheric Chemistry and Physics: From Air Pollution to Climate Change. Wiley, New York, 1998.

143

5. ATMOSPHERIC PHOTOCHEMISTRY

Wang, W.-C., and I. S. A. Isaksen, eds., Atmospheric Ozone as a Climate Gas. General Circulation Model Simulations. Springer-Verlag, Berlin, 1995. Warneck, P., Chemistry of the Natural Atmosphere. Academic Press, New York, 1988. Wayne, R. P., Chemistry of Atmospheres, 3rd ed., Oxford University Press, Oxford, U.K., 2000. Zellner, R., guest ed., Global Aspects of Atmospheric Chemistry. Steinkopff, Darmstadt, Germany, 1999.

EXERCISES 5.1. (a) Give the values for the molecular quantum numbers L and S for each of the ®ve electronic states of molecular oxygen shown in Figure 5-1. (b) For each of these ®ve states, state whether (1) interchange through the center of symmetry, and=or (2) interchange through the plane of symmetry, leads to a change in sign of the electronic wave function. (See Appendix A.) (c) Based on the selection rules for radiative absorption given in Section 5.1, which of the four electronic transitions between the ground state of molecular oxygen and the four excited states given in Figure 5-1 are allowed transitions? Justify your answer. 5.2. From Figure 5-2, determine the absorption cross section s of O2 at 160 nm. (Note that the vertical scale is logarithmic.) 5.3. Punta Arenas, Chile, is located at 538S latitude, which is at the edge of the Antarctic ozone hole (Section 5.2.3.3). On October 4, 1995, the column ozone concentration was 325 DU; on October 13, it had dropped to 200 DU [V. W. J. Kirchkoff et al., J. Geophys. Res., 102, 16109±16120 (1997)]. (a) Calculate the fraction of solar radiation intensity I=I0 transmitted by atmospheric ozone at 297 nm on October 4 and on October 13. The spectrum of ozone is given in Figures 5-3 and 5-4. (b) Calculate the percent increase in intensity at 297 nm from October 4 to October 13. 5.4. The thermodynamic equilibrium constant for the reaction M O ‡ O2 ! O3 is given by the expression
 12, 786 lnK atm 1 ˆ T

15:32

(a) Calculate the equilibrium constant at the temperature of the atmosphere at an altitude of 25 km (Figure 5-5). (b) The pressure of O2 is about 0.005 atm at 25 km, and the concentration of ozone is given in Figure 5-5. Calculate the ratio of the equilibrium pressure of O atoms divided by the equilibrium pressure of O2 …PO =PO2 †, at 25 km.

144

EXERCISES

(c) Would you expect this ratio to increase or decrease in the presence of sunlight? Why? 5.5. Using Figures 5-2, 5-3, and 5-5, calculate the percent of light transmitted at 205 nm by: (a) One meter thickness of molecular oxygen at an altitude of 25 km (where the pressure of O2 is 0.005 atm) and (b) one meter thickness of ozone at an altitude of 25 km. (c) From the calculations in parts a and b, which of these two species would you infer contributes more to absorption in the UV window of Figure 5-7 at 205 nm? Make a rough estimate of the percent of solar radiation transmitted by the stronger absorber at 205 nm from the outer atmosphere to 25 km. (Hint: To calculate the column concentration, assume that its concentration decreases linearly from the value at 22 km to 0 at 50 km; therefore the average concentration from 22 km to 50 km is half the concentration at 22 km, and 0 above 50 km.) 5.6. Show that the appropriate combination of reactions (5-29), (5-36), (5-37), and (5-39) gives the Chapman cycle, equation (5-41). 5.7. Both mechanisms (5-48) and (5-49) lead to the catalytic destruction of ozone. What is the signi®cance of one mechanism relative to the other? 5.8. (a) Devise a chain mechanism in which hydrogen atoms catalyze the destruction of ozone in the lower stratosphere. (b) Is water a reasonable source of H atoms in your mechanism? If so, why? If not, why not? (See Section 5.2.4.) 5.9. What is meant by the polar vortex? Why is it considered to be an essential feature of the Antarctic ozone hole? 5.10. What is the role of polar stratospheric clouds (PSCs) in the formation of the Antarctic ozone hole? 5.11. Explain in each case why the HCFCs and the PFCs have much lower ODPs than the CFCs. 5.12. What is the role of temperature inversion in photochemical smog? 5.13. Although the results of a photochemical smog chamber experiment shown in Figure 5-11 qualitatively agree in many ways with an actual case of photochemical smog (Figure 5-9), there are some signi®cant differences between the two sets of data. In particular, note that the ozone concentration increases to a constant amount in Figure 5-11, whereas it decreases signi®cantly after reaching a maximum in Figure 5-9. Discuss what might be the reason for this difference. 5.14. Calculate the percent of 397.5-nm light that would be absorbed by NO2 in a polluted atmosphere that is 1000 ft thick and contains the maximum concentration of NO2 given in Figure 5-9. Assume the pressure is constant at 1 atm and the temperature is 858F (29.48C).

5. ATMOSPHERIC PHOTOCHEMISTRY

145

5.15. (a) What are VOCs? (b) What is the role of VOCs in the production of photochemical smog? 5.16. It is stated that NO2 , formed mainly from NO, is the main light absorber in the atmosphere leading to photochemical smog. Give several examples of reactions involving the oxidation of NO to NO2 in an urban atmosphere. 5.17. We have seen that PAN, a component of photochemical smog, is thermodynamically unstable, decomposing into NO2 and the peroxyacetyl radical CH3 C…O†O2 . [the reverse of reaction (5-111)]. This reaction is very sensitive to temperature changes; at 258C the half-life of PAN is 27.5 mins, while at 1008C it is 0.18 s. (a) Calculate the rate constants (in s 1 ) at 258C and at 1008C. (b) Assuming that the empirical Arrhenius equation (4-24) is followed, calculate the activation energy Ea for the decomposition reaction.

6 PETROLEUM, HYDROCARBONS, AND COAL

6.1 INTRODUCTION Organic compounds are abundant in the environment, both as the products of natural, mainly biological, activity and as waste materials and pollutants from industrial processes. Organic compounds generally may be considered to be substituted hydrocarbons that are made up of straight or branched chains, rings, or combinations of these structures. The hydrocarbon skeletons are modi®ed by the presence of multiple bonds and substituents (oxygen, nitrogen, halogen, etc.) that markedly in¯uence the reactivity of the molecules. Unsubstituted hydrocarbons are relatively inert, particularly toward the polar compounds in the environment. All hydrocarbons are thermodynamically unstable with respect to oxidation to CO2 and H2 O, but the rate of this process is very slow except at elevated temperatures. However, the energy released by reaction with oxygen (about 12 kcal=g or 4500 J=g for saturated hydrocarbons) is very important for the generation of heat and electricity and for transportation in our industrial society. Organic compounds are the basis for life on earth. The synthesis of organic compounds in living systems is catalyzed by other organic substances called 147

148

6.2 THE NATURE OF PETROLEUM

enzymes. The degradation of organic compounds often follows a pathway that is the reverse of the synthesis, and the reactions are catalyzed by the same or similar enzymes. Many microorganisms utilize simple organic compounds for their growth, and their enzymes are responsible for the degradation of these substances. As a consequence, any compound that is synthesized by a living system is readily degraded biologically and is said to be ``biodegradable.'' However, many of the carbon compounds that have been formed by geochemical reactions (crude oil, coal) or industrial chemical processes (polyethylene, DDT) are not readily degraded and are frequently regarded as pollutants. These compounds will accumulate in the environment unless their degradation is catalyzed by a microbial enzyme or they are rendered more susceptible to enzymatic degradation by some other environmental process discussed in Section 8.2. These environmental processes are effective only insofar as they render the pollutant more susceptible to biodegradation by introducing appropriate functional groups that can serve as points of microbial attack. Since hydrocarbons are considered to be the parent compounds for organic materials, we shall consider them in this chapter. Coal, a potential source of hydrocarbons, is also discussed. Other organic compounds will be considered in later chapters. No attempt is made to deal with the general chemistry of the various classes of compounds and functional groups except as these reactions are important environmentally. It is assumed that the reader has some familiarity with the properties of hydrocarbons and their simple substituted derivatives.

6.2 THE NATURE OF PETROLEUM Crude oil is the predominant source of the hydrocarbon compounds used for combustion and for industrial processes, although as the supply of crude oil decreases, coal, oil shale, and tar sands may become more important sources of liquid and gaseous hydrocarbons. Crude oil is also a major source of environmental pollution. It is estimated that 2±9 million metric tons (tonnes) of crude oil and hydrocarbons enter the environment each year. Crude petroleum is a complex mixture of hydrocarbons that is separated into fractions of differing boiling ranges by the re®ning process shown schematically in Figure 6-1. The various fractions either are used directly as energy sources (``straight-run gasoline'') or are modi®ed chemically to yield more ef®cient energy sources such as high-octane gasoline. In addition, hydrocarbons may be converted to petrochemical compounds such as monomers, polymers, and detergents that are derived from petroleum.

149

6. PETROLEUM, HYDROCARBONS, AND COAL

Refluxing heat exchanger

Vapor Exchange Preheater

Pump Crude oil Decanter

Fractionating bubble tower

Gasoline Water

Cooler Steam Kerosene Pump Vapor

Vaporizer

Cooler

Slide stream receivers to give sharp fractions

Steam Gas oil Cooler

Heating furnace

Live steam

Wax distillate

Fuel oil FIGURE 6-1 Diagram of a crude oil distillation unit. The crude oil enters at the upper right-hand corner of the diagram and the products are taken off below on the right. Redrawn with permission of Scribner, a Division of Simon & Schuster, Inc., from The Chemistry of Organic Compounds, Fourth Edition by James Bryant Conant and Albert Harold Blatt. Copyright # 1952 by Macmillan Publishing Company. Copyright renewed # 1980 by Grace R. Conant.

Sulfur, oxygen, nitrogen, and metal derivatives are also present in petroleum, and compounds containing these elements are emitted when petroleum is burned. Sulfur is the most important minor constituent because it is emitted into the air as sulfur oxides when petroleum is burned, and the sulfur compounds released poison the catalytic converter on automobiles (Section 6.7.3). The sulfur content of crude oil ranges from 0.1 wt% for low-sulfur to greater than 3.7 wt% for high-sulfur petroleum. The sulfur is present mainly in the form of thiophene or thiophene derivatives such as the following:

150

6.3 SOURCES OF CRUDE OIL AND HYDROCARBONS IN MARINE ENVIRONMENTS

H3C

N CH2CH3

S Thiophene

S

H3C

2,3-Benzthiophene

S

2-Ethyl-4,5-dimethylthiazole

Nitrogen from nitrogen compounds constitute a much smaller percentage (
1% by weight) of petroleum than do sulfur compounds. The nitrogen is also present in the form of derivatives of the heterocyclic ring systems such as thiazole or substituted quinolines. CH3 N

N

S

CH3

CH3 Thiazole

2,3,8-Trimethylquinoline

Metals are present in petroleum either as salts of carboxylic acids or as porphyrin chelates (Chapter 9). Aluminum, calcium, copper, iron, chromium, sodium, silicon, and vanadium are found in almost all samples of petroleum in the range of 0.1±100 ppm. Lead, manganese, barium, boron, cobalt, and molybdenum are observed occasionally. Chloride and ¯uoride also are commonly encountered. Some of these metallic components are probably introduced into the petroleum when it is removed from the ground. The use of emulsi®ed brines and drilling muds (mixtures of iron-containing minerals and aluminum silicate clays) may account for the presence of some of these trace elements.

6.3 SOURCES OF CRUDE OIL AND HYDROCARBONS IN MARINE ENVIRONMENTS 6.3.1 Introduction The major environmental effects of petroleum are due either to crude oil itself or to the automobile hydrocarbon emissions from the gasoline fraction of the crude oil. Oil spills are generally associated with the release of hydrocarbons to the oceans or other water bodies, where much of the oil ¯oats and spreads over large areas of the water surface. Spills on land tend to be more easily contained to small areas, but they may result in the contamination of soil and local water supplies. This has been an important problem in cases of storage tanks that leak petroleum into the underground environment over long period of time. The primary environmental problems associated with spills in bodies of water

151

6. PETROLEUM, HYDROCARBONS, AND COAL

Big spills

37

Routine maintenance

137

Down the drain

363

Up in smoke Offshore drilling Natural seeps

92 15 62

FIGURE 6-2 The annual input of petroleum hydrocarbons into marine environments annually in millions of gallons: Big spills, major oil tanker and oil well accidents; Routine maintenance, bilge cleaning and other discharges from oil tankers and other large ships; Down the drain, used automobile engine oil, runoff from land of municipal and industrial waste; Up in smoke, hydrocarbons from vehicle exhaust and other sources that are rained out in the oceans; Offshore drilling, Spill from offshore oil wells; Natural seeps, oil seeping into the oceans from natural, underground sources. Redrawn from http:==seawifs.gsfc.nasa.gov=OCEAN_PLANET=HTML=peril_ oil_pollution=html.

are the effects of the slowly degraded petroleum residues on aquatic life. Automobile emissions, on the other hand, cause atmospheric problems. Much spilled oil also enters the atmosphere by evaporation, but the problems associated with oil spills and automobile emissions are suf®ciently different to warrant separate discussion in this chapter. The additional environmental problems of the surfactants, polymers, and pesticides synthesized from petroleum are discussed in subsequent chapters. It is estimated that the crude oil input into the sea is 7  108 gal=year worldwide (Figure 6-2). The sources of the oil, with the exception of delivery from the atmosphere, are discussed in the subsequent sections of this chapter. The atmospheric input is too diverse and ill de®ned to permit a clear delineation of all the sources.

6.3.2 Natural Sources Natural oil seeps led to the discovery of many of the major oil ®elds in the world. The ®rst oil well in the United States was drilled in Titusville, Pennsylvania, because oil was observed seeping into the Oil River at that point. These oil seeps may be responsible for local environmental problems, but often the rate of seepage is so slow that the oil is effectively dispersed by environmental

152

6.3 SOURCES OF CRUDE OIL AND HYDROCARBONS IN MARINE ENVIRONMENTS

forces. A major oil seep, 3600 gal=day, is at Coal Oil Point near Santa Barbara on the coast of southern California. This seep produces an extensive oil slick on the ocean and often results in tar accumulation on the shore. The oil also supports a community of marine microorganisms that metabolize these hydrocarbons. Most seeps produce less than 40 gal=day and the environmental effect appears to be quite limited. The contribution of natural sources to the oil in the marine environment is 9% of all sources. In 2000, earth-imaging satellites and radar discovered extensive natural seepage of oil into the Gulf of Mexico. It is estimated that the annual amount of oil released per year is twice that of the Exxon Valdez spill (2  11 million gallons: Section 6.4.1). This is a gradual release of oil, which wildlife is used to, and it forms a slick on the water 0.01 mm thick, which is of little danger to wildlife and is readily metabolized by bacteria. Some of these seeps have been occurring for thousands of years, and it has been proposed that there are food chains nurtured by the oil released by the seeps.

6.3.3 Offshore Wells Leakage from offshore oil wells is responsible for only about 2% of the oil in the sea (Figure 6-2). Thus it is surprising that there is always major opposition from local communities when it is proposed to drill for oil along the East or West coasts of the United States. This mind-set is probably due to the images of the well that ``blew'' off Santa Barbara, California, in January 1969. This oil was pressurized by methane gas in the ground, and the pressure forced out the oil when the well was drilled. The high pressure forced oil out of the sea¯oor in the vicinity of the well and thus the ¯ow could not be stopped by capping the well. It was necessary to drill additional wells to dissipate the gas pressure so that the oil ¯ow could be controlled. Other examples include the North Sea blowout in 1977 and the Ixtoc 1 well, which continued for almost a year (from June 1979 to the spring of 1980) in the Gulf of Mexico off the coast of Campeche, close to the Yucatan Peninsula. The latter well spewed out 140 million gallons of crude oil (Figure 6-3). Now, however, unless the oil is pressurized, potential ``blowout'' sites can be identi®ed by geologists, so the danger of major leaks from offshore oil wells appears to be minimal. There are 6000 wells off the coasts of Texas and Louisiana with no reports of major spills. One study has concluded that drilling offshore wells results in less environmental risk than transporting the oil in large tankers from the Gulf of Mexico or the Middle East because of the problems with tanker use discussed in Section 6.3.5.1 1

W. B. Travers and P. R. Luney, Science
, 791±796 (1976).

6. PETROLEUM, HYDROCARBONS, AND COAL

153

FIGURE 6-3 The Ixtoc exploratory well, which blew out and caught ®re June 3, 1979. It spilled 140 million gallons of oil into the Gulf of Mexico. From http:==www.nwn.noaa. gov=sites=hazmat=photos=ships=08.html. Also see color insert.

6.3.4 Industrial and Municipal Waste It is estimated that 51% of the oil in the marine environment is a result of industrial and municipal waste (Figure 6-2). About 1400 million gallons of used oil is generated each year in the United States. Most of this oil was used as a lubricant for automobile engines (crankcase oil) or as industrial lubricants. A large portion of this used oil is collected by commercial recyclers for direct use as fuel or for rere®ning into new oil. It is estimated that 363 million gallons of this used oil ends up in the environment (Figure 6-2). Automobile lubricating oil, changed by the vehicle owner, is a major source of the oil that is dumped or discarded in land®lls. About 50% of the 190 million gallons of oil that is changed by do-it-yourselfers is brought to collection centers such as gasoline stations. The other 95 million gallons is either sent to land®lls, dumped on the ground, or poured down storm sewers. This oil migrates through the soil and ®nally ends up in underground aquifers, rivers, lakes, and oceans. Until recently, used oil was sprayed on dirt roads to control dust but this practice was forbidden in 1992 because such oil contains toxic metals and toxic hydrocarbons that had been rapidly leached into water supplies. California has an aggressive program of collecting and recycling oil. Of the 137 million gallons of used oil generated each year in the state,

154

6.3 SOURCES OF CRUDE OIL AND HYDROCARBONS IN MARINE ENVIRONMENTS

over half (83 million gallons) is collected. This program has resulted in noticeable decreases in the levels of oil present in soil and water samples in the state. There have been major concerns raised concerning the burning of 800 million gallons of used oil each year to heat schools, hospitals, apartment buildings, and factories in the United States. The combustion of this oil is not regulated because it is not classi®ed as hazardous. It is not labeled as hazardous because this would stigmatize the oil, causing people to be less willing to recycle it. Yet it contains lead, chromium, cadmium, and other toxic constituents, and many of these are emitted into the atmosphere during the combustion process. For example, in 1992 it was estimated that about 600,000 lb of lead compounds was released during the combustion process, an emission rate greater than any other industrial process. Oil cannot be legally combusted if it contains more that 100 ppm lead, but this standard is 10 times higher than the limit for other fuels imposed by the U.S. Environmental Protection Agency (EPA). Used oil that is to be burned must be tested ®rst to determine that the levels of lead, chromium, cadmium, benzene, and other constituents are within the EPA standards for these substances. If not, the used oil is usually blended with other oil so that the mixture meets EPA standards.

6.3.5 Transportation The major source of oil in the marine environment is spills resulting from crude oil transport. There are some 6000 oil tankers worldwide that transport crude oil, and these vessels are designed to ride low in the water when carrying a full load. After they unload their cargo they must take on seawater as ballast for their return trip to the oil ®elds. This ballast is pumped into holding ponds where the oil can be recovered. However, this ballast, along with the residual crude oil in their tanks, is pumped into the ocean before the next cargo of crude oil is loaded. It is estimated that 0.4% of the capacity of a tanker sticks to the tanker wall after the crude oil is discharged. If the tanker takes on ballast equivalent to one-third of its total capacity then about 16  104 gal of crude oil will be pumped out with the ballast of a tanker having a capacity of 12  106 gal. It is estimated that every year 137 million gallons of oil is introduced into the sea from ``routine maintenance'': ejection of tanker ballast and the many small spills resulting from crude oil transport (Figure 6-2). The sea lanes around the continent of Africa and the subcontinent of India are the most heavily oiled in the world as a result of the spills from the dense tanker traf®c leaving the Persian Gulf (Figure 6-4).

155

6. PETROLEUM, HYDROCARBONS, AND COAL

80⬚

40⬚

0⬚

40⬚

80⬚

160⬚

120⬚

80⬚

40⬚

0⬚

40⬚

80⬚

120⬚

160⬚

FIGURE 6-4 Positions at which visible oil slicks were observed between 1975 and 1978 by the Interglobal System Marine Pollution (Petroleum) Monitoring Project. Redrawn from E. M. Levy, M. Ehrhardt, D. Koknke, E. Sobtchenko, T. Suzuoki, and A. Tokuhiro, Intergovernmental Oceanographic Commission, UNESCO, 7 Place de Fontenoy 75700, Paris, France 1981. Used by permission of the United Nations.

6.3.6 Catastrophic Oil Spills Catastrophic oil spills can have dramatic local environmental effects, and because of this they are well documented in the national press and television. Major oil spills became a problem on the east coast of the United States in World War II when German submarines sank over 60 oil tankers, releasing 65  105 metric tons of oil over a period of three years. Since the tankers were traveling close to the shore in an attempt to avoid the submarines, much of this oil eventually washed up on the beaches. Today major oil spills occur each year as a result of oil tanker accidents (Figure 6-2). The huge tankers (Figure 6-5) release vast amounts of oil when accidents occur. These accidents are inevitable because of the steady stream of tankers traveling from the oil-producing centers in the Middle East and Alaska (Figure 6-4), just as automobile accidents are inevitable on busy highways. Catastrophic spills contribute only about 5% to the total amount of oil entering the marine environment as a result of transportation, but they have a

156

6.3 SOURCES OF CRUDE OIL AND HYDROCARBONS IN MARINE ENVIRONMENTS

FIGURE 6-5 The ``midsize'' oil tanker Ventiza, built in 1986. It is 247 m (811 ft, or 2.7 U.S. football ®elds) long and 41.6 m (136 ft) wide. In 2000 the largest tanker in the world was the Jahre Viking, which is 458 m (1504 ft, or 5 U.S. football ®elds) long and 69 m (266 ft, or 0.89 U.S. football ®eld) wide. From http:==www.rigos.com=ventiza.html. Also see color insert.

major impact on the local environment if the oil reaches the shore. Catastrophic spills will occur less frequently if more double-hulled tankers (vessels having a 9- to 10-ft buffer area between the two hulls) are used. If an accident perforates the outer hull, there is a reasonable probability that the inner hull will not be breached and no oil will be released. Federal legislation passed in 1990 requires oil tankers proceeding between two destinations in the United States to have double hulls and mandates the removal from service of singlehull tankers over 25 years old. There has been an upsurge worldwide in the use of double-hulled tankers. This increase is probably due more to the potential for costly ligation resulting from an oil spill than to the laws passed by the U.S. Congress. There has been a decrease in the amount of oil spilled since 1984 (Figure 6-6; see also Table 6-1). Oil tankers and other big ships have been identi®ed as a major source of air pollution. These ships burn high-sulfur fuels that release large amounts of sulfur dioxide (SO2 ) and nitrogen oxides (NOx ) as well as particulates into the air. The EPA plans to regulate these emissions, but international agreements will be required to enforce any such regulations. As noted earlier, oil spills on land are more readily contained and are usually a less serious environmental problem than those at sea. One notable exception

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6. PETROLEUM, HYDROCARBONS, AND COAL

500,000,000 450,000,000

Annual gallons spilled

400,000,000 350,000,000 300,000,000 250,000,000 200,000,000 150,000,000 100,000,000 50,000,000

1998

1996

1994

1992

1990

1988

1986

1984

1982

1980

1978

1976

1974

1972

1970

1968

0

FIGURE 6-6 Oil spills over 10,000 gal (34 tonnes) since 1968. The major oil spills decreased in the 1984±1998 period. The 240 million gallons deliberately released in Kuwait during the Gulf war was the principal contributor to the total amount spilled in 1991. Redrawn from D. S. Etkin, International Oil Spill Statistics: 1998. Cutter Information Corp., Arlington, MA. Copyright # 1999. Used by permission of Cutter Information Corporation.

TABLE 6-1 Oil Spills In Order of Amount Spilleda 1. 26 January 1991: terminals, tankers; 8 sources total; sea island installations; Kuwait; off coast in Persian Gulf and in Saudi Arabia during the Persian Gulf War (240.0) 2. 03 June 1979: Ixtoc I well; Mexico; Gulf of Mexico, Bahia del Campeche (140.0) 3. 02 March 1990: Uzbekistan, Fergana Valley (88) 4. 04 February 1983: platform no. 3 well; Iran; Persian Gulf, Nowruz Field (80.0) 5. 06 August 1983: tanker Castillo de Bellver; South Africa; Atlantic Ocean, 110 km northwest of Cape Town (78.5) 6. 16 March 1978: tanker Amoco Cadiz; France; Atlantic Ocean, off Portsall, Brittany (68.7) 7. 10 November 1988: tanker Odyssey; Canada; North Atlantic Ocean, 1175 km northeast of St. Johns, Newfoundland (43.1) 8. 19 July 1979: tanker Atlantic Empress; Trinidad and Tobago; Caribbean Sea, 32 km northeast of Trinidad-Tobago (42.7) 9. 11 April, 1991: tanker Haven; Genoa, Italy (42) 10. 01 August 1980: production well D-103 (concession well); 800 km southeast of Tripoli, Libya (42.0) (continues)

158

6.4 FATE OF AN OIL SPILL

TABLE 6-1 (continued) 11. 12. 13. 14. 15. 16. 17. 18. 19. 20. 21. 22. 23. 24. 25.

02 August 1979: tanker Atlantic Empress; 450 km east of Barbados (41.5) 18 March 1967: tanker Torrey Canyon; United Kingdom; Land's End (38.2) 19 December 1972: tanker Sea Star; Oman; Gulf of Oman (37.9) 23 February 1980: tanker Irene's Serenade; Greece; Mediterranean Sea, Pilos (36.6) 07 December 1971: tanker Texaco Denmark; Belgium; North Sea (31.5) 23 February 1977: tanker Hawaiian Patriot; United States; Paci®c Ocean 593 km west of Kauai Island, Hawaii (31.2) 20 August 1981: storage tanks; Kuwait; Shuaybah (31.2) 25 October 1994; pipeline: Russia; Usinsk (in area that was closed to foreigners before collapse of Soviet Union) (30.7) 15 November 1979: tanker Independentza; Turkey; Bosporus Strait near Istanbul, 0.8 km from Hydarpasa port (28.9) 11 February 1969: tanker Julius Schindler; Portugal; Ponta Delgada, Azores Islands (28.4) 12 May 1976: tanker Urquiola; Spain; La CorunÄa Harbor (28.1) 25 May 1978: pipeline no. 126 well and pipeline; Iran; Ahvazin (28.0) 05 January 1993: tanker Braer; United Kingdom; Garth Ness, Shetland Islands (25.0) 29 January 1975: tanker Jakob Maersk; Portugal; Porto de Leisoes, Oporto (24.3) 06 July 1979: storage tank tank no. 6; Nigeria; Forcados (23.9) a

Number in parentheses refers to millions of gallons spilled. Source: excerpted from D. S. Etkin, International Oil Spill Statistics: 1998. Cutter Information Corp., Arlington, MA, 1999. http:==www.cutter.com=oilspill

was the ¯ooding caused by Hurricane Agnes in 1972, which resulted in the release of 6±8 million gallons of sludge and oil from storage tanks in Pennsylvania.

6.4 FATE OF AN OIL SPILL The dispersal of an oil spill is illustrated in Figure 6-7. When oil is spilled, the lower boiling fractions evaporate and dissolve rapidly, with the result that 25±50% of a crude oil spill is soon lost from the surface of the sea. The extent to which these processes occur is determined by the temperature of water and the intensity of wind and wave action. The residue of higher molecular weight hydrocarbons is slowly degraded by microorganisms. This process may be slow because the other nutrients needed for growth, especially nitrogen, are quite limited in the ocean. In addition, the insoluble petroleum contains molecular species that are too large to be assimilated through the cell walls of microorganisms and will undergo biodegradation only after the petroleum has been broken down into smaller molecules by a combination of photochemical and oxidative processes. As a general rule, microorganisms cannot assimilate

159

ap or ati on

6. PETROLEUM, HYDROCARBONS, AND COAL

Ev

Atmospheric oxidation

Aerosol tion forma

Rain and fallout

Bulk surface discharge thick layer of oil

Water-in-oil emulsions “chocolate mousse” Spreading

Sea surface oil slick

C

Oil-in-water transformation emulsion Absorption Chemical onto degradation particulate matter Dispersed

d an n io g ct lin ve el on upw

Dissolution Globular Solubilizing dispersion chemical

crude oil

Tarry lumps

Carbon cycle

Ocean

Biodegradation Assimilation into marine food chain

Nonbuoyant oil residues

Biological detritus

Bulk subsurface discharge

Degradation or assimilation by benthic organism

Seafloor sediments

FIGURE 6-7 Fate of spilled oil. Redrawn with permission from R. Burwood and G. C. Speers, Estuarine and Coastal Marine Science, Vol. 2, pp. 117±135. Copyright # 1974. Used by permission of Academic Press.

organic molecules of molecular weight greater than 500 Da. Consequently the remaining higher molecular weight material is whipped up into a ``mousse'' of hydrocarbons and water by waves and winds, and this mousse slowly breaks up into tar balls. These ¯oat unless mixed with enough sand to give them a density that exceeds the density of seawater in which case they sink to the bottom. Continued action of light, oxygen, and waves breaks the material up into smaller and smaller particles and to molecules that can eventually be degraded by microorganisms.

160

6.4 FATE OF AN OIL SPILL

6.4.1 Weathering of an Oil Spill The polycyclic aromatic hydrocarbons in crude oil sensitize the photochemical formation of singlet oxygen (Section 5.2.2), which oxidizes the ole®ns present to cyclic dioxides and hydroperoxides: O

O O H

+ O2 (1∆g)

O

6-1†

H OOH

+ O2 (1∆ g )

…6-2†

These compounds can either rearrange directly [equation 6-1] or be cleaved photochemically to form hydroxyl radicals OOH

O

hν

+ OH

…63†

that attack the other unsaturated molecules present: OO O2

+ OH

RH

+ H2O OOH

…64†

alcohols, phenols, carbonyl compounds, and acids + R

The net result of these radical processes is the solubilization of the polycyclic aromatic hydrocarbons by conversion to phenols, alcohols, carbonyl compounds, and acids. The breakup of the spill is slowed if it is washed up on the shore. Dispersal and degradation will continue if there is a strong wind and surf, but oil spills in quiet bays or lagoons may take 5±10 years to disperse in the absence of wave

6. PETROLEUM, HYDROCARBONS, AND COAL

161

and wind action. The toxic effects on marine life likewise persist for 5±10 years in these environments. The long-term effects of an oil spill are determined by the environment in which it occurs. Spills that never reach the shore have the least effect because most marine life tends to be near the land±sea interface, where food supplies are more abundant and ®sh travel to lay eggs and birds and amphibians raise their young. Thus a spill that remains at sea has less chance of damaging the eggs and rapidly developing young marine life, which are the organisms most susceptible to toxins of any sort.

6.4.2 Cleaning Up Oil Spills One initial reaction to an oil tanker accident is to send another tanker or barge to the leaking vessel and try to of¯oad the crude oil. Most tanker accidents, however, occur in stormy weather or as a result of hazardous conditions on the tanker. If this is the case of¯oading the crude is not feasible, and the ®rst action is to put out a boom to contain the spill. Then skimmers, or boats with the capability to collect surface oil, are sent out. Skimmers work with small spills in calm water but have been less effective in large spills such as the 11-million-gallon spill by the tanker Exxon Valdez in Prince William Sound, near Valdez, Alaska, in 1989. The skimmers used there had a very low capacity and could not take on the oil as fast as it was coming out of the tanker. In addition, when the skimmers had ®lled their tanks they were 3 hours from shore, where the pumping facilities were, and the 6-hour round trip also limited their usefulness. Later, when wave action in Prince William Sound increased, the ef®ciency of the skimmers decreased markedly because they passed over the oil without removing it. (Booms used to control the spread of the oil are effective only in calm sea.) The fate of the oil from the Exxon Valdez released into Prince William sound is shown in Figure 6-8. If the spill cannot be contained or collected, the next approach is to drop or spray dispersants on the oil to increase its miscibility with seawater. For example, dispersants were used to keep the toxic oil released by Ixtoc 1 in the Gulf of Mexico from reaching the shore. This treatment dispersed the oil in micelles. The dilution of the oil diminished the concentrations of the toxic hydrocarbons, and the dispersed oil underwent more rapid biodegradation than it would have as a separate layer on the surface. Studies of the toxic effects of this spill were limited, but there were no reported effects on the size or quality of the shrimp catch in that part of the Gulf of Mexico. The one danger with dispersants is their possible toxic effects on marine biota. For example, the phenolic dispersants used on the oil spilled from the Torrey Canyon in 1967 were more toxic than the crude oil. Recent studies have

162

6.4 FATE OF AN OIL SPILL

Atmospheric photolysis 20%

Beached 2% Recovered 14%

Subtidal sediment 13% Dispersed in water 1%

Biodegraded/photolysed in water 50%

FIGURE 6-8 Fate of the oil from the Exxon Valdez spill of 1989 in Prince William Sound, near Valdez, Alaska. Redrawn from http:==www.oilspill.state.ak.us=beaches=beaches=htm. Also see color insert.

identi®ed detergents that are less toxic to marine life than crude oil but equally effective in dispersing the spill. One treatment that is seldom used today is the addition of agents like chalk, which cause the oil to sink to the bottom. This approach has been abandoned because the precipitated petroleum has a long lifetime in the bottom sediments, where the dissolved oxygen content is low. There the persistent hydrocarbons have a toxic effect on marine life for many years. The hydrocarbons may also change an aerobic environment to an anaerobic one, which inhibits the degradation of the petroleum by aerobic microorganisms. Once the oil reaches the shore, a variety of techniques may be used to either collect the oil or wash it off the beaches. A spray of hot seawater was used to ¯ush the oil from the Exxon Valdez off the rocks and beaches of Prince William Sound, and the oil released was collected from the surface of the water near the shore. This treatment may have been more detrimental than helpful. The number of microorganisms in the treated areas was found to be less than that present before treatment, suggesting that the treatment was more toxic to marine microbes than the oil. Bioremediation, a different approach to cleaning oil spills, was also investigated for the removal of oil from the beaches in Prince William Sound. Fertilizers were sprayed on the oily beaches to enhance the growth of the

6. PETROLEUM, HYDROCARBONS, AND COAL

163

oil-eating bacteria that occur in the natural environment. The fertilizer consisted of essential nutrients, such as nitrogen and phosphorus compounds that are present in only small amounts in the sea, mixed with emulsifying agents to solubilize the oil. These nutrients together with the carbon of the petroleum provide an environment in which petroleum-consuming bacteria can thrive. Inipol EAP 22, a mixture of oleic acid, lauryl phosphate, 2-butoxyethanol, urea, and water, appeared to be effective in enhancing the rate of loss of oil from beaches. In some instances a two- to ®vefold increase in the rate of biodegradation of the oil was observed, and there was a marked improvement in the appearance of the treated beaches in comparison to control areas where no Inipol was used. However, in one case the visual improvement was misleading, for analysis showed no difference in the amounts of oil on the treated beach and in a control area that had not been treated. Some studies were performed in an attempt to determine which of the components of the bioremediation mixture (Inipol EAP 22) were most effective in promoting bacterial degradation of oiled beaches in Prince William Sound. Nitrogen, which appears to be the limiting nutrient for hydrocarbonmetabolizing bacteria in the presence of an oil spill, is believed to be essential for bioremediation to be successful. The presence of oleic acid and lauryl phosphate stimulates the growth of other bacteria, including some nitrogen®xing ones, which enhance the growth of the hydrocarbon-metabolizing bacteria. Oleic acid and lauryl phosphate are added only initially, since their continued addition mainly supports the growth of bacteria that do not consume oil. Large colonies of bacteria that do not metabolize oil will consume the other essential nutrients (e.g., nitrogen) necessary for the oil eaters to grow. Detergents that tend to disperse the oil also enhance the rate of bacterial consumption of oil because it is easier for the bacteria to ingest the dispersed hydrocarbons. These factors have been evaluated qualitatively only because it is dif®cult to monitor the degradation of an oil spill in the ocean. Somewhat better data have been obtained for spills on beaches, but these data probably are not directly applicable to an oil slick on the ocean. At present there are no data showing that addition of known oil-metabolizing bacteria accelerates the degradation of the spill. The current view is that there is a bloom of oil-metabolizing bacteria as soon as the oil is spilled, and thus there is no need to add more bacteria. Addition of nitrogen- and phosphorus-containing fertilizers enhances the growth of the bacteria, which results in the rapid biodegradation of the oil. Too much fertilizer should be avoided, since this results in the proliferation of microorganisms that do not metabolize the oil but do deplete the molecular oxygen in the water. The oil-eating bacteria are aerobic, so the depletion of oxygen will slow their growth.

164

6.5 EFFECTS OF CRUDE OIL ON MARINE LIFE

6.5 EFFECTS OF CRUDE OIL ON MARINE LIFE The population of marine microorganisms that can metabolize soluble hydrocarbons increases dramatically in the vicinity of an oil spill. The growth of these microorganisms in the ocean is limited by the hydrocarbon content of the water, so they multiply at a much greater rate when there is a big increase in the hydrocarbon content of the seawater. As noted earlier, nitrogen is the growthlimiting nutrient in the presence of excess hydrocarbons. Almost all forms of life absorb hydrocarbons and are affected by crude oil. The acute toxicity (an imminent health hazard) of crude oil is proportional to the percentage and structures of the aromatic compounds present. Soluble aromatic hydrocarbons containing two or more condensed rings have the highest acute toxicity. Ingestion of crude oil by birds and mammals inevitably leads to their death. The bulk of the oil ingested is a result of an animal's attempts to remove the oil from feathers or fur. Ingestion is also a consequence of eating oiled plants or animals. For example, seals can easily catch and eat oiled birds that are unable to ¯y. Plants and coral reefs are also susceptible to the toxic effects of crude oil. Sea grasses and mangrove forests have been killed by crude oil. Birds and mammals are weakened by oil that binds fur or feathers together. This greatly decreases the insulating capacity of the fur or feathers, with the result that the animals lose heat at a much more rapid rate than before. Consequently they must eat much more food to maintain their body temperature. This is a serious problem for mammals like polar bears and sea otters, which spend a lot of time in the sea and are unable to escape from the vicinity of the spill. These animals also experience eye irritation as a consequence of their surfacing in the oil and getting it in their eyes. Laboratory studies and other studies have demonstrated that crude oil is more toxic to eggs and developing young marine life than it is to adults. Such studies also indicate that marine life does not instinctively avoid oil spills. The toxic effects of the crude oil appear to be short-lived. Most marine life repopulates a previously affected area within one to two years, and there is little visible effect on the ecosystem. The rate of recovery is strongly dependent on the activity of the ocean on the shoreline. In areas where there is active surf, the ocean constantly scrubs the beach and the rocks, and the oil is dispersed. Oil spilled in a protected area may persist for many years, so it takes correspondingly longer for the environment to return to its prespill condition. The indirect effects of oil spills are not well known, but these are potentially as important as the direct effects just noted. It is known that ®sh and other forms of marine life are stimulated in their search for food, in their escape from predators, and in their mating by the organic compounds in the sea. The messages received by the ®sh may be masked by the presence of

6. PETROLEUM, HYDROCARBONS, AND COAL

165

petroleum, or the compounds present in the crude oil may convey incorrect messages. We now turn to some of the numerous laboratory studies to determine the effects of crude oil on various types of marine life as well as observations made at the sites of oil spills.

6.5.1 Fish Laboratory studies have shown that dissolved hydrocarbons destroy the membranes in gills, which results in a diminished ability to absorb oxygen from the water. This loss of gill ef®ciency results in an enlarged heart. There is also less ef®cient utilization of food, an effect that may be related to diminished adsorption of food through the intestinal walls. The proposed decrease in food adsorption may also be due to damage to the lipid layers in the intestines. The diminished populations of bottom-feeding ®sh in the vicinity of some spills suggests that these may be affected most. This may be due to ingestion of oil adsorbed on the sediments.

6.5.2 Clams, Mussels, and Other Invertebrates There is usually a sharp decrease in the populations of invertebrates in the vicinity of oil spills because, unlike ®sh, they do not have suf®cient mobility to move away from the area of the spill and they live in sediments that contain adsorbed oil. These mollusks absorb oil into their systems, where it inhibits the production of eggs and sperm, causing an abrupt drop in their populations. Oil is also toxic to the adults, as shown by the large quantities of dead mollusks, crabs, and sea urchins that washed up on the shores of France after the Amoco Cadiz spill. The populations of these invertebrates gradually build up again over a period of several years.

6.5.3 Birds The oiling of birds is usually one of the most dramatic visual effects of an oil spill. The toxicity of the oil ingested during a bird's attempts to remove the oil from its feathers usually results in the death of the animal. Very few of the birds recover, in spite of heroic efforts by rescue workers. There appear to be no long-term effects on the bird population; their numbers rebound rapidly within a year or so. For example 35,000 dead birds were retrieved as a consequence of the Exxon Valdez spill, and the total death toll was much higher±close to 200,000 birds, including about 200 adult bald eagles. However in one year's

166

6.5 EFFECTS OF CRUDE OIL ON MARINE LIFE

time it was observed that a signi®cant number of birds occupied areas that had been oiled and, more speci®cally, 51% of the bald eagle nests in the oiled region were occupied and produced an average of 1.4 eaglets per nest, the usual ratio for this area. It was demonstrated that ingestion of sublethal amounts of crude oil by herring gull chicks causes several sublethal effects that could impair the ability to survive. In this study the chicks suffered liver effects and ceased to grow in comparison to similar chicks that had not ingested oil. A similar study on young herring gulls and puf®ns showed oxidative damage to the hemoglobin of their red blood cells. Thus it appears unlikely that birds that have been subjected to a large amount of oil will survive for long even if the oil covering their feathers is removed. These birds will have ingested oil in their attempts to remove it from their feathers and consequently will be subject to its sublethal toxic effects.

6.5.4 Sea Otters and Other Marine Mammals: Marine animals (like sea otters are very susceptible to the toxic effects of the oil mainly because they spend most of their time in the sea, swimming and surfacing through the oil. Exxon expended $8 million dollars for the helicopter capture of 357 otters ($80,000 per otter!), of which 234 survived. Many of the captured otters were not oiled or were only slightly oiled. Those that survived were cleaned and released, 45 with surgically implanted radio monitors. Only 22 of those with radio monitors were detected the following spring, suggestive of a high mortality rate. In addition, 878 dead otters were found, and it is likely that many more dead otters were never recovered. A report published in 2000 noted that sea otters born after the 1989 Exxon Valdez oil spill in Prince William Sound had a lower rate of survival than sea otters born before the oil spill. This suggests that the young are still experiencing the toxicity of the oil 8±10 years later. These ®ndings show that, as in the case of birds, it does not make sense to expend ®nancial and human resources to try to rescue and resuscitate oiled mammals. Given the toxic effects of the oil, coupled with the stress the animals experience as a result of the capture, cleaning, and release process, there are very few survivors. Necropsies revealed severe emphysema (probably from the oil fumes) as well as liver, kidney, intestinal, and bone marrow abnormalities. It is likely that ingestion of crude oil will have the same effects on other mammals, including humans, since the same physiological effects were observed in laboratory studies on the effects of crude oil on rats. The one exception is oiled penguins (Figure 6-9). A survival rate, exceeding 90%, in comparison to the normal survival rate of nonoiled penguins, is reported for the African penguins oiled by spills at the tip of Africa.

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FIGURE 6-9 Oil drips from the tail of a severely oiled African penguin. Photograph from http:==www.uct.ac.za=depts=stats=adu=oilspill=pic02.htm. Copyright # L. G. Underhill, 2000. Used by permission of the University of Cape Town on behalf of L. G. Underhill. Also see color insert.

6.5.5 Sea Turtles Laboratory studies on sea turtles were performed because the young hatch on the beach and must swim from the shore through the ocean. Since those that hatch on the African or Indian coasts must swim through the sea lanes where there are large amounts of crude oil (Figure 6-4), laboratory studies were carried out to determine the effects of sublethal doses of crude oil. Young turtles that had to surface to breath through an oil slick that was 0.05±0.5 cm thick developed pretumorous changes, lesions, and swelling over a period of 2±4 days. When there was the option of surfacing in the presence of the oil or in an area where there was no oil, the turtles did not avoid the oil. These ®ndings suggest that there may be long-term toxic effects on the young as they swim through the sea lanes. They may not encounter the high concentrations

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6.6 USE OF PETROLEUM IN THE INTERNAL COMBUSTION ENGINE

of oil in the laboratory experiments, but they will be in contact with it for longer periods of time.

6.6 USE OF PETROLEUM IN THE INTERNAL COMBUSTION ENGINE One of the major uses of petroleum as an energy source is in the automobile internal combustion engine. Most automobiles are driven by a fourstroke-cycle piston engine (Figure 6-10). Gasoline is mixed with air in the carburetor and drawn into the cylinder on the ®rst stroke. The oxygen±gasoline vapor mixture is compressed on the second stroke and ignited by the spark plug. The expanding gases formed by combustion then drive the piston down on the third stroke, the stroke that provides the power to drive the car, and the combustion products are forced out of the cylinder on the fourth stroke. The ®rst automobiles had low-compression engines that could use the gasoline fraction distilled from crude oil (Figure 6-1), but as the automobile was improved, more powerful engines were developed. These high-compression engines required a more sophisticated fuel than straight-run gasoline. In high-compression engines, the hydrocarbons of simple petroleum distillates preignite before the top of the stroke of the compression cycle. Preignition decreases engine power because it results in an increase in the pressure on the piston before it has completed the upward stroke of the compression cycle. The preignition usually occurs explosively (knocking), which jars the engine and hastens its eventual demise. The octane rating of gasoline is a measure of its tendency for preignition and detonation. The higher the research octane number (RON), the less likely that

Stroke 1

Stroke 2

FIGURE 6-10 Schematic of a four-stroke-cycle engine.

Stroke 3

Stroke 4

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6. PETROLEUM, HYDROCARBONS, AND COAL

knocking will occur. The octane rating is an empirical number that is measured on a standard test engine. It relates to the performance of the automobile engine when it is operating at low to medium speeds. The RON values of some representative compounds are listed in Table 6-2. The values of 0 for nheptane and 100 for isooctane were established as arbitrary standards. A variation of the octane scale designated motor octane number (MON) is also used to rate gasolines. The MON scale was established when it was observed that there was not good agreement between the RON determined in a test engine and that of the motor run under road conditions. The higher speeds and heavier weight of contemporary automobiles resulted in lower octane ratings in road tests than were observed in the test engine. The same test engine is used for both the MON and RON, but the operating conditions for MON determination give octane ratings that correlate more closely with those observed with an engine running at medium to high speed. The octane rating listed on gasoline pumps is an average of the RON and MON. It should be emphasized that octane ratings do not measure the energy released on combustionÐall hydrocarbons release about the same amount of energy per gram when burned completelyÐbut instead are a measure of the tendency for preignition and explosive combustion. A number of methods have been developed to increase the RON rating (55±72) of straight-run gasoline. It was discovered in 1922 that the RON of straight-run gasoline could be increased to 79±88 by the addition of 3 g of ``lead'' per gallon. The ``lead'' or ``ethyl ¯uid'' that is added to gasoline is a mixture of about 60% tetraethyl lead [Pb…CH2 CH3 †4 ], and=or tetramethyl lead [Pb…CH3 †4 ], about 35±40% BrCH2 CH2 Br and ClCH2 CH2 Cl, and 2% dye, TABLE 6-2 Research Octane Numbers (Octane Ratings) for Some Representative Hydrocarbons Compound n-Octane n-Heptane n-Hexane n-Pentane 2,4-Dimethylhexane Cyclohexane n-Butane 2,2,4-Trimethylpentane (isooctane) 2,2,4-Trimethylpentene-1 Benzene Toluene a

Standards for RON measurement.

RON 19.0 0a 24.8 61.7 65.2 83 93.8 100a 103 106 120

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6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE

solvent, and stabilizer. The lead prevents preignition by binding to hydroperoxyl free radicals, reactive intermediates with unpaired electrons, formed in the combustion process: RH ‡ O2 ! R
‡
OOH

…6-5†

This quenching decreases the combustion rate and prevents preignition. Leaded gasoline is no longer used in the United States and is discussed further in Section 6.7.4. Catalytic re-forming, the conversion of aliphatic compounds to aromatic compounds, is the process of isomerization of linear aliphatic hydrocarbons to cyclic derivatives that are then dehydrogenated to aromatics as shown in reaction (6-6). The reaction pathway is determined by the nature of the binding of the hydrocarbons to the surface of a platinum or platinum-rhenium catalyst that is used. A product with a RON of 90±95 is obtained. In reaction (6-6), n-heptane is used to illustrate the cyclic compounds proposed as intermediates in the catalytic re-forming process. CH3 CH3(CH2)5CH3

CH3

CH2CH3 +

+ + H2

CH3

+ 3H2

…6-6†

CH3

Ethanol and other oxygenated organic compounds that enhance the octane hydrocarbon mixtures are discussed in Section 6.7.4. Apparently when compressed in the cylinder of the automobile engine, the substituted aromatics and oxygenated organics also react with hydroperoxyl and other free radicals to inhibit the preignition of gasoline vapors.

6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE 6.7.1 Introduction Some hydrocarbons are natural components of the atmosphere. For example, most of the atmospheric methane is produced by anaerobic bacteria in swamps and bogs, and in the stomachs and intestines of cows, sheep, and termites; a much smaller percentage is released by natural gas wells. It has been proposed that many of the hydrocarbons found in the Gulf of Mexico may be due to the marsh plants indigenous to the Gulf Coast. Many plants, especially conifers and citrus, release terpenes into the atmosphere. It has been suggested that the

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171

6-day air pollution alert in the Washington, DC, area in August 1974 was due mainly to the presence of terpenes originating from plants in the Appalachian Mountains. In the absence of any man-made pollution, there would be still parts-per-million concentrations of methane (Table 2-1) and parts-per-billion amounts of ethane, ethylene, acetylene, and propane in the atmosphere.

6.7.2 Hydrocarbons and Other Emissions from Automobiles The automobile is a major nonnatural source of hydrocarbons in the atmosphere. The photochemical reactions of its gasoline and exhaust gases is an important source of an array of atmospheric oxidants that cause eye irritation and other problems for animals and plants (Section 5.3). Automotive air pollution is caused by the evaporation of gasoline or by tailpipe emissions. Gasoline evaporation occurs during the ®lling of the gas tank, and by the heating and cooling the automobile, as a result of diurnal temperature changes, and by operating the vehicle. In California and other areas of the country, vapor recovery systems connected to the gas tank collect the vapor displaced when it is ®lled. The displaced hydrocarbons are captured in canisters of activated carbon and later released into the engine during operation of the vehicle. Tailpipe emissions from automobiles have been reduced signi®cantly as a result of federal legislation, and this has resulted in a signi®cant increase in air quality (Chapter 5). In 1968 the federal government decided to control automobile emissions by imposing standards for new cars (Table 6-3). It was assumed that older cars that did not meet the emission standards would eventually wear out and be taken off the road. The allowed emissions for new cars were continually lowered until 1981, and were unchanged during the 1981±1993 time period. Emission standards were further lowered starting in 1994. The legislated emissions from new cars were decreased by more than a factor of 10 between 1968 and 1994, and these reductions resulted in a decrease in air pollutants (Table 6-4). The most dif®cult source of emissions to control is that from the exhaust pipe. This is because the internal combustion engine, as it is presently designed, will always emit some noncombusted hydrocarbons. The main source of these hydrocarbons is ``wall quench'' in the engine. The burning of the gasoline close to the walls of the cylinder is quenched because the zone next to the wall is much cooler than the combustion zone in the center of the cylinder. This relatively cold area slows the rate of combustion so that the hydrocarbons in this region are swept out by the piston before combustion is complete. Wall quench also occurs in the crevice above the piston rings between the cylinder wall and the piston (Figure 6-11). There would still be hydrocarbon emissions from the automobile even if it were possible to eliminate wall quench. This is because there is insuf®cient

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6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE

TABLE 6-3 Maximum Emissions from New Automobiles Hydrocarbons (g=mi) Before controlsa 1968 1970±1971 1972 1973±1974 1975±1976 1977 1978±1979 1980 1981±1993 1994 2004

CO (g=mi)

10.60 6.30 4.10 3.00 3.00 1.50 1.50 1.50 0.41 0.41 0.25 0.125

84.0 51.0 34.0 28.0 28.0 15.0 15.0 15.0 7.0 3.4 3.4 1.7

NOx (g=test) 4.1 (6.0)b

3.0 3.1b 2.0 2.0c 2.0 1.0 0.4 0.2

Evaporation (g=test) 47

2 2 6 6 2 ±

a

Average values before legislation. Emissions of NOx increased with control of HCs and CO. There was no NOx standard at that time. c Change in test procedure. Source: Adapted from J. G. Calvert, J. B. Heywood, R. F. Sawyer and J. H. Seinfeld, Science, 
, 37±44 (1993). b

time for the complete combustion of gasoline to carbon dioxide and water. Addition of more air (oxygen) to the engine allows more complete combustion, but this results in an increase in the NOx emissions (Figure 6-12) and a decrease in the power (Figure 6-13). The increase in NOx is due to the higher

TABLE 6-4 Percent Decrease of Six Pollutants between 1975±1985 and 1986±1995 Pollutant Pb CO SO2 Particulates NOx O3

1975±1985 93 47 46 20 17 14

1986±1995 78 36 37 17 14 6

Source: Council on Environmental Quality, 22nd Annual Report, Washington, DC, March 22, 1992, p. 10, and Chem. Eng. News, pp. 22±23, Jan. 6, 1997.

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6. PETROLEUM, HYDROCARBONS, AND COAL

Spark plug Intake valve

Exhaust valve

Wall and crevice quench

Piston

Piston ring

FIGURE 6-11 Regions of wall and crevice quench in the cylinder of a four-stroke cycle internal combustion engine.

12

3000

2000

8

CO HC

4

1000

Nitric oxide concentration (10−6)

Hydrocarbon concentration (10−4 C6) Carbon monoxide concentration (%)

NO

S

0

0 10

18 14 Air/fuel ratio by weight

22

FIGURE 6-12 Effect of air/fuel ratio on hydrocarbon (HC), carbon monoxide (CO), and nitric oxide (NO) exhaust emissions; S, stoichometric operation. Redrawn from W. Agnew, Proc. R. Soc. Ser. A. , 153 (1968). Used by permission of The Royal Society of Chemistry.

174

6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE

Maximum power

Specific fuel consumption

Best economy air/fuel ratio

Power

Best power air/fuel ratio

Power

Fuel consumption

Best economy 9

10

11

12 13 14 Air/fuel ratio

15

16

17

FIGURE 6-13 Effect of air=fuel ratio on power and economy. Redrawn from W. Agnew, Proc. R. Soc. Ser. A. , 153 (1968). Used by permission of The Royal Society of Chemistry.

temperature of the combustion zone in the engine in the presence of more oxygen. Automobiles that travel farther on a gallon of gasoline are less polluting. In addition, they conserve valuable fuel resources. In 1978 the U.S. government instituted a program setting an average mileage goal for the ¯eet of cars manufactured by the major automobile companies. This corporate average fuel economy (CAFE) was gradually increased from 18 miles per gallon (mpg) in 1978 to 27.5 mpg in 1985. The U.S. Congress and presidents have been unwilling to increase the CAFE since 1985 because of concerns regarding the increased cost of the high mileage automobiles, and because the lighter cars that would have to be used might not protect their occupants in collisions as well as heavier vehicles. Environmental groups claim that the technology is

6. PETROLEUM, HYDROCARBONS, AND COAL

175

available to produce a ¯eet of cars that average 45 mpg, but there is strong resistance to such a mandated increase from automobile manufacturers. The environmentalists were correct, since both conventional and hybrid gasoline± electric cars with mileage in the 40±50 mpg range were introduced in the United States in 2000.

6.7.3 The Catalytic Converter Since the internal combustion engine, as presently designed, cannot operate without producing emissions, some device must be added to the automobile if both NOx and hydrocarbon and carbon monoxide emissions are to be controlled. In 1973 recirculation of the exhaust gases was introduced to help control NOx emissions. In addition, in some cars air was injected into the hot exhaust gases to facilitate continued oxidation of hydrocarbons. In 1975 in the United States, 85% of the new cars sold were equipped with a catalytic reactor in the exhaust stream to catalyze the oxidation of CO and hydrocarbons. Lead added to gasoline poisons the catalysts in the catalytic converter; therefore, starting with the 1975 models, all cars equipped with a catalytic converter were required to use lead-free gasoline. The catalytic converter has evolved from a device that simply catalyzed the conversion of carbon monoxide and hydrocarbons to carbon dioxide, to a single unit that uses the reducing capacity of the gases emitted from the engine to ®rst reduce NOx to N2 and then later to oxidize the reduced gases to carbon dioxide upon addition of air: 2HC ‡ CO ‡ 2NOx ‡ …3x O2 † ! 3CO2 ‡ H2 O ‡ N2

…6-7†

2HC ‡ CO ‡ 3O2 ! 3CO2 ‡ H2 O

…6-8†

In 1979 the catalyst was a mixture of mainly platinum, rhodium, palladium, and ruthenium on a thin ®lm of alumina coated on a honeycomb of ceramic or on ceramic pellets (Figure 6-14). Because of the expense of using platinum and rhodium, the catalyst evolved to being mainly palladium by 1997. This was made possible by higher engine temperatures, which minimize the deactivation of the palladium due to deposition of sulfur and phosphorus on its surface. The extent of oxidation of hydrocarbons and CO and the reduction of NOx depends on the composition of the gases coming from the engine. If the engine is operating at an air=fuel ratio less than stoichiometric (reducing conditions, Figure 6-12), the ef®ciency for NOx reduction is higher but the conversion of HC to CO2 is less ef®cient. If the engine is operating at an air=fuel ratio higher than stoichiometric (oxidizing, Figure 6-12), the conversion of NOx to N2 is less ef®cient but the oxidation of hydrocarbons and CO is more ef®cient. There is a very small air=fuel window near the stoichiometric ratio for the optimal

176

6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE

Insulation

Ceramic honeycomb catalyst

Insulation cover

Outlet Inlet

Shield Coating (alumina) + Pt/Pd/Rh

O, NO

HC, C

Substrate

Catalyst halfshell housing Intumescent mat

FIGURE 6-14 Cutaway view of an automotive catalytic converter. The honeycomb (enlarged, bottom left) contains 300±4000 square channels per square inch on which the metal catalysts are coated. Emissions pass through these channels and react on the catalyst surface. Provided by R. J. Farrauto, Engelhard Corp., NJ.

effectiveness of the catalytic converter. Ideally engines could be operated under oxidizing conditions that would permit ef®cient fuel consumption, resulting in the consumption of most of the hydrocarbons and CO. At the present time, however, there is no practical way to eliminate the NOx formed in the absence of a reducing agent to convert it to N2 . The 1990 amendments to the Clean Air Act mandated that emissions be reduced to even lower levels by 2004 and that the catalytic converter have a useful life of 100,000 rather than 50,000 miles. Emission standards more stringent than the national ones have been adopted by California and eleven northeastern and middle Atlantic states. A major step toward meeting the new emission standards will be the development of a catalytic converter that is operative when the engine is initially started. About 50% of the emissions from an automobile engine, as measured in a standard test procedure, are emitted during the ®rst 100 s when the catalytic converter is being brought to its operating temperature of 400±6008C. Placement of the catalytic converter closer to the engine will result in a faster warm-up, but the converter will have to be reengineered to operate at about 10008C, a temperature at which

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177

the present catalysts are inactivated and the ceramic core is not stable. In addition, the reduction of NOx is less ef®cient at higher temperatures. One possible solution is to electrically heat a portion of the catalyst when the car is started. The catalyst in a forward compartment of the converter would be coated on a metallic core that can be electrically heated to 4008C in 5 s by using power from the alternator. The remainder of the catalyst would be layered on a porous ceramic core as shown in Figure 6-14. Other possible solutions include the development of catalysts that are active at lower temperatures and the use of zeolites and other materials placed in the exhaust line before the converter, which adsorb the gaseous emissions when cold and release them when the operating temperature of the converter is reached. Meeting the requirement that the catalytic converter last for 100,000 miles will also require new catalyst formulations that are not poisoned by zinc, phosphorus, and sulfur, as are the present formulations. These elements are present in zinc dithiophosphate, a compound added to lubricating oil for the reduction of engine wear. Finally, there is active research on the development of better catalysts for the reduction of NOx . This would make it possible to run the car engine at an air=fuel ratio of 18±21 instead of the stoichiometric conditions used currently (Figure 6-13). An air=fuel ratio of 18±21 results in the more complete combustion of gasoline to carbon dioxide and greater fuel economy as well.

6.7.4 Gasoline Additives: Tetraalkyllead, Ethanol, and Methyl tert-Butyl Ether Tetraalkyllead compounds (mainly tetraethyl- and tetramethyllead), the antiknock compounds in lead ¯uid, the main antiknock additive in gasoline since the 1920s, are no longer used in the United States. The phaseout of lead in gasoline in the United States took place between 1975 and 1995. The Environmental Protection Agency initiated this phaseout mainly because of the adverse effect of lead on the catalytic converter, but also because of the possibility that the lead emissions from automobiles may be a health hazard (Section 10.6.10). In 1968, the combustion of leaded gasoline was responsible for 98% of the 185,000 tons (166,500,000 kg) of atmospheric lead in the United States. It is estimated that 7 million tons of lead was released to the environment from the use of this additive between 1923 and 1986. Removing lead from gasoline has resulted in a major decrease in atmospheric lead (Table 6-4). For example, lead deposition in the White Mountains of New Hampshire decreased from 31 to 1±2 g=hectare in the 1975±1989 period (1 hectare ˆ 104 m2 ). In addition, there was a 76% decrease in the average blood lead level in U.S. residents from 1976 to 2000. Other studies have shown that up to 50% of the blood lead is due to the ingestion of atmospheric lead produced by leaded gasoline. It is well known that lead compounds are toxic, especially to children, so the removal of lead from

178

6.7 SOURCES OF HYDROCARBONS AND RELATED COMPOUNDS IN THE ATMOSPHERE

gasoline should enhance the general health of the population. Unfortunately tetraethyllead is still used in the gasoline of many developing countries and in eastern Europe. Aromatic organics, which have high octane ratings (Table 6-2), can be used in place of lead ¯uid to enhance the octane rating of straight-run gasoline. Being more toxic than aliphatic hydrocarbons, these aromatics constitute a health hazard when inhaled in large amounts, so other octane enhancers have also been used. The deleterious health effect due to aromatics in gasoline, however, is much less than the combined hazards of lead and organic emissions from cars without catalytic converters. Ethanol is also used as an octane enhancer for petroleum; the 7±10% mixture in gasoline is often called gasohol. The action of ethanol as an octane enhancer was discovered in 1917, and at that time General Motors scientists proposed that it be used as a gasoline additive. A General Motors researcher discovered the antiknock effect of tetraethyllead in 1921, and the compound was selected as the approved additive by GM and Du Pont executives in 1923. They chose tetraethyllead instead of ethanol because the former, as a new material, it could be patented. The health hazards of lead compounds were known at the time, but tetraethyllead was chosen because money could be made on the patent. More recently gasohol was introduced because it can be produced by fermentation of biomass, mainly corn in the United States, and its incorporation into gasoline decreases the country's dependence on imported crude oil. Ethanol, derived from the fermentation of sugar, is not only used as a gasoline extender in Brazil, but is also used directly as a fuel. In 1991 ethanol constituted about 25% of the fuel used to power vehicles in Brazil and about one-third of these vehicles used only ethanol. The use of ethanol decreased in 1989±1991 mainly because of discoveries of crude oil in Brazil, which resulted in cheaper gasoline. The addition of ethanol to gasoline in the United States is subsidized by the government to aid midwestern farmers. A disadvantage of ethanol is that it is hygroscopic and it picks up traces of water when gasoline that contains ethanol is shipped in pipelines. Since water is detrimental to automobile engines, ethanol must be shipped separately to local distributors, where it is blended with gasoline just before use. These two steps add to the cost of gasoline that contains ethanol. More recently, another oxygenated organic compound, methyl tert-butyl ether (MTBE), has been used to enhance the octane rating of gasoline. It, together with ethanol, has the additional advantage of decreasing carbon monoxide (CO) emissions. As a consequence, the EPA has mandated the use of these or other oxygenated organics (``oxygenates'') in U.S. cities in which the daily CO levels exceed the air quality standards prescribed by the Clean Air Act. The U.S. consumption of MTBE was 4 billion gallons a year in 1998, with one-third of the use in California. In the winter of 1992±1993, in cities where gasohol or gasoline containing 15% MTBE were used, there was an 80% drop

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179

in the number of days in which the CO emissions exceeded the national standard in comparison to the winter of 1991±1992. Concerns with regard to the detrimental health effects of MTBE arose in the early 1990s. While MTBE has been used as an octane enhancer since 1979, when it was used in large amounts in 1992 in Fairbanks and Anchorage, Alaska, there were many reports of headaches, nausea, dizziness, and irritated eyes. In subsequent years, there were similar complaints from some of the residents of Colorado, California, New Jersey, North Carolina, Maine, and Wisconsin. More recently MTBE has been found in groundwater, where it imparts a noxious odor to drinking water when present in amounts greater than 3 ppb, although at the time of writing there are no de®nitive data on health hazards resulting from its ingestion. The rapid transport of MTBE in groundwater is due to its high solubility in water. It was estimated in 1999 that 250,000 gasoline stations in the United States had leaky underground storage tanks and that these are the source of the groundwater contamination. As of 2000, several states had banned the use of MTBE as a gasoline additive, and the EPA was planning a gradual phaseout of its use as an octane enhancer and as an additive for the reduction of carbon monoxide emissions. Ethanol appears to be the principal additive that will be used to reduce CO emissions in urban areas if the use of MTBE is banned. One can only imagine the health problems associated with lead and possibly MTBE that would have been avoided if ethanol had been chosen as the antiknock agent in 1923. Another antiknock agent, methylcyclopentadienylmanganese tricarbonyl (MMT), has been used in Canada since about 1970. Long-term health effects have not been fully evaluated, and there is considerable debate concerning the possible deleterious effect of this additive on the engine monitoring equipment, which results in an increase in hydrocarbon emissions. The Canadian government had decided to discontinue the use of MMT because of possible neurotoxicity and interference with pollution-monitoring systems. In response to a lawsuit from the manufacturer based on the claim that the ban violated the North American Free Trade Agreement, however, the use of this additive was reinstated in 1998. Lawsuits also resulted in reapproval of MMT for use in the United States in 1995, although despite the lifting of the ban, addition of this antiknock agent to gasoline in the United States had not resumed as of 2000.

6.8 THE AIR POLLUTION PROBLEM IN URBAN CENTERS In spite of the advances made in automobile emission control, air pollution is still a problem in urban centers. The daily ambient air levels of CO were exceeded periodically in 42 cities in 1991, and the corresponding ozone levels were exceeded frequently in 9 cities. Los Angeles continues to have high levels of photochemical smog and ozone, air pollution problems that are more severe

180

6.8 THE AIR POLLUTION PROBLEM IN URBAN CENTERS

than almost any other U.S. city. Currently the American city with the greatest air pollution is Houston, Texas. This continued urban pollution is initially surprising, considering that tailpipe emissions from new cars have been cut more than 10±fold over the 1968±1993 time period. Although the automobile emission standards for new cars have been lowered markedly, air sampling studies in highway tunnels, where other sources of polluted air are minimal, have shown that the average automobile emissions have not decreased as much as the mandated tailpipe emissions. For example, there has been only a threeto fourfold decrease in hydrocarbon and carbon monoxide and only a two- to threefold decrease in NOx in the 1968±1993 time period (Table 6-3). Tests on individual automobiles show that about 50% of the emissions come from 10% of the automobiles. Older automobiles have higher emissions. These cars were made when emission standards were more lenient, and they have catalytic converters with diminished or no ability to effect a decrease in tail pipe emissions. The higher emission rate of these older cars is partially offset by the lower number of miles they are driven annually in comparison to new cars. Surprisingly, about 20% of the new cars in every model year are high emitters. About 30% of these have had their emission controls intentionally disabled, and the emissions controls in the other 70% of such cars are not operating because they have not been properly serviced. It should be possible to solve these problems by providing incentives to replace old cars with newer models and mandating periodic checks of emission systems. Others factors also contribute to the continued urban air pollution. One is that the miles driven in urban environments have doubled in the past 25 years. Another is emissions from stationary sources. For example, oil re®neries, power plants, dry cleaning businesses, and auto repair shops emit hydrocarbon solvents, while restaurants and homes give off emissions from stoves, furnaces, ®replaces, lawn mowers, and grills. These sources, plus the natural emissions of terpenes from citrus and other plants, are becoming more important components of the photochemical smog in Los Angeles now that contributions from automobiles are decreasing.

6.8.1 Plans to Reduce Auto Emissions in Urban Centers Several approaches are available to improve the quality of air in areas of high population density. Reformulated gasolines that have lower volatilities and use additives such as MTBE and ethanol to reduce CO emissions will probably be used. A catalytic converter that catalyzes the degradation of pollutants when the car is ®rst started probably be mandated, as well. Alternative fuels, lowemission fuels such as natural gas, will be used in ¯eets of cars like taxis that operate in cities. In California in 1998, there was a requirement that 2% of all vehicles sold have zero tailpipe emissions. This percentage is mandated to

6. PETROLEUM, HYDROCARBONS, AND COAL

181

increase to 10% by 2003. Other measures, such as stricter controls on the stationary sources mentioned earlier and limiting the number and types of vehicles in downtown areas, will also be implemented until the levels of carbon monoxide, ozone, volatile organics, and nitrogen oxide are decreased to the standards set by the federal EPA and by the state of California.

6.8.2 Low-Emission Automobiles The adoption of vehicle emissions standards in California that are more restrictive than the national standards has forced the U.S. automobile companies to develop automobiles that have very low emissions and to produce zero-emission vehicles (ZEVs) as well. At present the only ZEVs are electrically powered, and there is a major emphasis in this area since the adoption by eleven eastern states of the California emission standards. The ZEVs must be an increasing number of the vehicles each auto-maker sells each year, starting in 2003. Strictly speaking, electrically powered cars do not emit pollutants during operation, but electricity from a power plant, which has emissions (see Chapter 15), is required to charge their batteries. Studies carried out in 1992 show that the emissions resulting from the use of electric vehicles will be much lower than those from gasoline-powered automobiles even when the emissions from the power plants are taken into account. The net decreases in emissions for the electric car versus the gasoline-powered car are as follows: carbon dioxide, 2-fold; NOx , 6-fold; volatile organics, 100fold, and carbon monoxide, 200-fold. These decreases are possible because the emissions from power plants are controlled more readily than the emissions from thousands of automobiles. A small added bene®t of the use of electric vehicles will be a decrease in consumption of oil used to power automobiles. Since oil is used to generate little of the electric power (5%) in the United States, the use of electric cars will not have signi®cant impact on this need. In 1999, however, the advantage of lower emissions from electric vehicles appeared to be decreasing in magnitude as new designs for catalytic converters for gasoline-powered automobiles resulted in lower emissions for these vehicles. Problems presently associated with electric vehicles include the short distance traveled, about 200 miles, before the battery needs charging, the long charging times, the weight of the bank of batteries required, the high cost of the vehicle in comparison to a gasoline-powered one of the same size, and the relatively short lifetime of the batteries (30,000±50,000 miles). In addition, if the electric vehicles are powered by lead batteries, there is a strong possibility of increased lead in the environment. None of these problems appear to be insurmountable at the present time. For example, it is possible in California to ``®ll up'' an electric vehicle in parking lots, at ``gas'' stations, and at parking meters, and to pay by credit card. Two manufacturers

182

6.9 COAL

introduced ZEVs in the United States in 2000. For the reasons just cited, however, they have not been popular. Vehicles with low and ultralow emissions are also prescribed in the California regulations. These will include hybrids, vehicles mainly powered by electricity but with the capability of also being powered by an internal combustion engine under certain driving conditions, such as steep hills or rapid acceleration. This engine, running in its most ef®cient mode, is also used to maintain the battery charge. Taxi ¯eets may be powered by natural gas and buses by fuel cells. Fuel cells generate power by the electrochemical oxidation of hydrogen or hydrocarbons, with up to 80% conversion of the chemical energy to electrical power. Very low emissions of carbon monoxide and NOx are produced in these controlled oxidations (Section 15.9). Two manufacturers have introduced hybrid vehicles in the United States that use gasoline ef®ciently and generate very low emissions. These hybrids have gasoline mileage in the range of 40±50 mpg which is about the same as that of some conventionally powered vehicles of the same size. Most large trucks and buses are powered by higher boiling diesel fuel (kerosene and light oil) (Figure 6-1), not gasoline. The diesel engine is similar to the internal combustion engine of the automobile except that the fuel is not ignited by a spark plug when compressed. Ignition proceeds as a result of the heat generated on compression of the air=fuel mixture. This combustion is not as fast as that resulting from the ignition of vapors by a spark, and uncombusted carbon, which is emitted as a black smoke containing particulates of carbon with adsorbed hydrocarbons, remains in the diesel cylinder. The 1990 amendments to the Clean Air Act mandated a sixfold decrease in these particulates in the 1991±1994 time period, along with reduction in the NOx levels. In 1997 the U.S. Environmental Protection Agency decided to extend its regulation of particulate emissions to particles 2.5 mm or greater in diameter. This was prompted by studies that noted a correlation between the level of atmospheric particulates and their associated sulfates with death rates. The studies noted an increase in heart and lung disease with the amounts of 2.5-mm particles in the air. This proposal drew a strong negative reaction from an industrial trade association but was supported by an independent study group. The EPA plans to obtain more de®nitive data on the distribution of these particles in the environment before it proposes speci®c regulations for their emissions. It is estimated that these proposals will be issued around 2010.

6.9 COAL 6.9.1 Coal Formation and Structure Coal was probably the ®rst of the fossil fuels to be used for energy. It was recognized as an energy source by the Chinese around 1100 b . c ., while the

6. PETROLEUM, HYDROCARBONS, AND COAL

183

ancient Greeks were probably the ®rst of the western cultures to be aware of coal. The Romans reported that the ``¯ammable earth'' was being mined in Gaul when they captured that section of Europe. The ®rst known coal mines in North America were operated by the Hopi Indians of Arizona some 200 years before Columbus. Coal occurs mainly in the north temperate regions of the earth. Small deposits are located at the poles, but there are almost none in the tropics. The bulk of the world's deposits are located in Siberia in the former Soviet Union (
50%) while signi®cant amounts are found in the United States (
25%) and China (
15%). Coal was formed from the debris of giant tree ferns and other vegetation that grew in swamps and bogs 300 million years ago. When the plants died they were covered with sediment that prevented their oxidation by atmospheric oxygen. Further buildup of sediment and other geological processes subjected these materials to high pressures that resulted in their conversion to the solid, ¯ammable substance we know as coal. There are several classes of coal that re¯ect different stages in the metamorphosis from the carbohydrate and lignin of plants to the carbon of anthracite coal. Peat, a substance of a low heat value, is formed in the ®rst stage of the process as a result of anaerobic microbial transformations of plant material. The lignin and microbial remains in the peat gradually lose H2 O and CO2 as a result of high temperatures and pressures and are converted successively to lignite, bituminous coal, and anthracite. Anthracite, or hard coal, is about 85% carbon, with the remainder being mainly inorganic material and water. The carbonization of plant carbohydrate results in the formation of a highly condensed aromatic ring structure similar to graphite. Aliphatic rings and chains as well as hydroxyl, carbonyl, carboxyl, and ether groupings are attached to these aromatic structures. Nitrogen, about 1% of the coal, is present as the cyclic amine function and sulfur as thiol (RSH), thioether (RSR), and disul®de (RSSR) groupings. Some of these structural elements are present in the postulated structure for bituminous coal (Figure 6-15). Oxidation of coal by aerobic bacteria removes some of the covalently bound organic sulfur. Coal contains a variety of inorganic ions that ultimately end up in the ash residue after the coal is burned. Some 36 elements were detected in the ash resulting from the burning of West Virginia bituminous coal, with the major constituents being Na, K, Ca, Al, Si, Fe, and Ti. Toxic compounds of arsenic, selenium, and mercury (Section 10.6.7) are released during coal combustion. Pyrite (FeS2 ), a major source of sulfur in coal, is not bound to the coal but occurs with it. It is formed by the action of anaerobic bacteria that reduce the sulfate in coal to sul®de [see reaction (11±21) in Chapter 11]. The sul®de reduces iron (III) to iron (II) with the corresponding oxidation of sul®de to S22 .

184

6.9 COAL

OH

SH

OH OH CH2 O

C H2 H OH

NH2

H2 H H2

O

S

H

H

S

O H

CH3 S

O

CH3

C C H2 H2

H CH2

C O OH

CH2 H

CH3

H

H

C C H2 H2

S

N

O

CH2

OH

H N

OH

O

CH2

CH2

CH2

HO

O

CH3

OH OH

CH2

O

H HO

H HO

H2 H

FIGURE 6-15 A postulated partial structure for bituminous (soft) coal. The stars indicate additional connecting points to the polymeric coal structure. Redrawn from N. Berkowitz, An Introduction to Coal Technology, 2nd ed. Academic Press, San Diego, CA. Copyright # 1994.

The combination of the two products yields pyrite (FeS2 ). The total sulfur content of coal is about 0.6±3.2% by weight, with approximately half of that sulfur due to the pyrite present.

6.9.2 Coal Gasi®cation The gasi®cation of coal was carried out extensively from about 1820 to 1920 for the production of coal gas, which was used for lighting (gaslights) and energy in the United States and elsewhere. However the discovery of abundant natural gas in the 1950s and the construction of pipelines to deliver the gas from the southern United States to the northeastern and western states resulted in the shift to the cleaner, cheaper natural gas as a fuel. As a consequence, the production of coal gas ceased and there were few new developments in coal gasi®cation until the 1970s, when petroleum shortages prompted renewed interest in the use of coal, the most abundant fossil fuel in the United States. Coal gasi®cation, the ®rst step toward the production of hydrocarbons from gasoline (Section 6.9.3.2), was used extensively by the Germans in World War

185

6. PETROLEUM, HYDROCARBONS, AND COAL

II when their access to petroleum was cut off. South Africa developed the technology further after World War II, and it was the source of 50% of their gasoline and related fuels. Gasi®cation by the Lurgi process (Figure 6-16) is used in South Africa and in the Great Plains gasi®cation facility in Beulah,

Coal lock Recycle tars Distributor drive

Steam

Water

Gas scrubber Product gas Distributor

Grate

Tar and water

Grate drive

Water jacket Steam and oxygen

Ash lock

FIGURE 6-16 Schematic drawing of a Lurgi pressure gasi®er. Redrawn from N. Berkowitz, An Introduction to Coal Technology, 2nd ed. Academic Press, San Diego, CA. Copyright # 1994.

186

6.9 COAL

North Dakota, a commercial plant that became operational in 1985. A number of other gasi®ers that appear to be more ef®cient than the Lurgi reactor have been developed but the low cost of natural gas forestalled the construction of commercial units based on this new technology until 2001, when the cost of natural gas increased sharply. The Great Plains facility was selling syngas at a pro®t in 2001. In the Lurgi process coal is added to the top of the reactor and steam and oxygen (not air) are injected into the bottom. The temperature in the reactor is 900±10008C and the pressure is 3±3.5 MPa. This ®rst step of the gasi®cation process produces a mixture of carbon monoxide and hydrogen called ``water gas'': 4C…coal† ‡ 2H2 O…steam† ‡ O2 …hot air† ! 4CO ‡ 2H2

…69†

The ``water gas'' has a heating value of about 300 Btu per standard cubic foot (scf), or (11.2 mJ=m3 ). In comparison, the heating value of natural gas (mostly methane) is 940 Btu=scf (35 mJ=m3 ). The pieces of coal, which must be larger than a quarter-inch, migrate to the bottom of the reactor as they burn, and the inorganic ash that remains goes through the grate into the ash lock, while the gases are removed near the top of the reactor. A portion of the CO formed is reacted with steam in a second step, to generate hydrogen: CO ‡ H2 O ! CO2 ‡ H2

…6:10†

This hydrogen, with that generated in reaction (6-9) is used in the third step to convert the remaining carbon monoxide to methane: CO ‡ 3H2 ! CH4 ‡ H2 O

…6:11†

Nitrogen and nitrogen compounds are converted to ammonia, which is removed by treatment with an acid wash and sold as fertilizer. Sulfur compounds are converted to hydrogen sul®de, which is oxidized to elemental sulfur or sulfate and sold. The operation of the Great Plains Gasi®cation Facility is discussed in Section 15.3.5. Considerable research has been performed on the gasi®cation of coal in the ground, a process that avoids the costly, dangerous, and potentially environmentally destructive extraction of coal by underground or strip mining. Research on this topic was initiated in the 1930s in the Soviet Union, and the initial procedures were worked out there. Underground gasi®cation was explored in the United States and Europe starting in 1945, but most of these projects were abandoned with the discovery of new sources of natural gas. In 1994 two operational facilities in the former USSR were producing gas for heating and power. One is in Angrensk, near Tashkent, and the other at Yuzhno-Abinsk near Novosibirsk. The basic process is shown schematically in Figure 6-17. The coal is ignited in the vicinity of the intake pipe(s) for air and

187

6. PETROLEUM, HYDROCARBONS, AND COAL

Product gas

Air

Overburden

Coal seam Combustion zone

Reduction zone

Pyrolysis zone

FIGURE 6-17 Schematic diagram of underground coal gasi®cation. Redrawn from N. Berkowitz, An Introduction to Coal Technology, 2nd ed. Academic Press, San Diego, CA. Copyright # 1994.

steam, and the products of partial combustion and reduction (mainly carbon monoxide, carbon dioxide, and hydrogen) are collected from the outlet pipe. The success of the venture depends on the size of the coal seam and its permeability. Often the permeability needs to be enhanced by fracturing the coal seam by forcing high-pressure water or passing an electric current through it. If the coal seam is thicker than 1.5 m, it is possible to use this process to extract energy with better than average ef®ciency in comparison to mining and to gasify better than 75% of the coal. The discovery of large Siberian supplies of natural gas in the 1950s in the Soviet Union resulted in the closure of several underground gasi®cation facilities and the cancellation of plans to build new ones.

6.9.3 Coal Liquefaction 6.9.3.1 Conversion of Mixtures of Carbon Monoxide and Hydrogen to Hydrocarbons

Reaction (6-12) gives the Fischer±Tropsch process for the hydrogenation of carbon monoxide in the presence of iron, cobalt, or nickel catalysts to form hydrocarbons. Fe

CO ‡ H2 ƒƒ! hydrocarbons

…6-12†

188

6.9 COAL

This process was investigated in the 1920s in Germany and was used in that country during World War II for the synthesis of fuel. The feedstock for the manufacture of gasoline was obtained by coal gasi®cation (Section 6.9.2). This same approach to fuel formation was adopted in the 1950s by South Africa, which has abundant coal supplies but no petroleum. About half of the annual petroleum requirements for South Africa are produced from 6 million tons of coal. This method of hydrocarbon formation is basically inef®cient, since all the bonds of coal are broken to form carbon monoxide, a partially oxidized product, and these carbon±carbon and carbon±hydrogen bonds are re-formed to produce hydrocarbons. It would be more ef®cient if the coal could be hydrogenated directly to hydrocarbons, a process we describe next. 6.9.3.2 Direct Conversion of Coal to Hydrocarbons

The ®rst studies on the direct conversion of coal to hydrocarbons were performed in the laboratory of F. Bergius in Germany in 1918±1925. This chemist developed what is known as the Bergius process, in which pulverized coal is slurried in oil with an iron catalyst and heated with hydrogen at 450±5008C to form a mixture of oils having medium (180±3258C) and high (>3258C) boiling points. The medium boiling oil is sent to a second reactor, where it is catalytically cracked (broken into smaller hydrocarbons) and further hydrogenated at 4708C and a pressure of 240±300 atm to yield gasoline and kerosene. The high boiling fuel oil is slurried with another batch of pulverized coal, and the cycle is repeated. The ®rst plant to carry out this process was constructed in Germany in 1927. Approximately a billion gallons of gasoline was produced in Germany by this process during World War II. The gasoline produced by the Bergius and related processes has a high octane rating because it consists of about 20±25% aromatic compounds, a re¯ection of the high proportion of aromatic structural units in coal. Research on the direct conversion of coal to hydrocarbons was dormant from the 1950s until the oil embargoes of the 1970s because of the low price and high availability of crude oil from the Middle East. Interest was rekindled by the oil boycott of 1973, and a number of variations of the Bergius process have been developed. Incremental improvements in the process have been made, and now greater yields of hydrocarbon products can be had at lower temperatures and hydrogen pressures (Table 6-5). Development is continuing at a plant in Wilsonville, Alabama, where a consortium of power companies, petroleum companies, and the U.S. government is sponsoring research. Other processes, which differ from the original Bergius process, have also been investigated by a number of petroleum companies. Most of these projects have been terminated because of the continued availability of low-priced crude oil.

189

6. PETROLEUM, HYDROCARBONS, AND COAL

TABLE 6-5 Evolution of Coal Liquefaction Technology Operating characteristics Pressure (MPa)a Max. temperature (8C) Coal conversionb Hydrogen consumptionb Hydrocarbons yieldb Distillable liquids yieldb

1935

1945

1980

69 480

21 465 94 8 25 54

21 455 94 6 11 51

14 30 54

1986 19 440 94 5.6 7 65

a MPa b

ˆ 106 pascals  10 atm. Wt % of moisture- and ash-free coal feed. Source: Data from R. E. Lumpkin, Science, , 873 (1988).

Additional Reading Fuels Derived from Oil Atlas, Ronald M., Slick solutions, Chem. Bri., pp. 42±45, May 1996. Courtright, Michael L., Improper disposal of used motor oil not only threatens the environment, it also wastes a valuable resource, Machine Design, , 81±86 (1990). Etkin, D. S., International Oil Spill Statistics: 1998. Cutter Information Corp., Arlington, MA., 1999, 66 pp. Glaser, John A., Engineering approaches using bioremediation to treat crude oil±contaminated shoreline following the Exxon Valdez accident In Alaska. In Bioremediation Field Experience, P. E. Flathman, D. E, Jerger, and J. H. Exner, eds., pp. 81±103. Lewis, Boca Raton, FI, 1993. Jackson, J. B. C., and 16 others, Ecological effects of a major oil spill on Panamanian coastal marine communities, Science 
, 37±44 (1989). Mielke, J. E., Oil in the Ocean: The Short-and Long-Term Impacts of a Spill. Congressional Research Service, Library of Congress, 90±356 SPR, July 24, 1990. Prince, Roger C., Petroleum spill bioremediation in marine environments, Crit. Rev. Microbiol.,
, 217±242 (1993). Smith, J. E., ``Torrey Canyon'' Pollution and Marine Life. Cambridge University Press, London, 1968. Steering Committee for the Petroleum in the Marine Environment Update, Oil in the Sea. Inputs, Fates and Effects. National Academy Press, Washington DC, 1985, 601 pp. Steinhart, C. E., and J. S. Steinhart, Blowout. A Case Study of the Santa Barbara Oil Spill. Duxbury, Belmont, CA, 1972. Tanker Spills: Prevention by Design. National Research Council, National Academy Press, Washington DC, 1991. Thayer, A. M., Bioremediation: Innovative technology for cleaning up hazardous waste, Chem. Eng. News, pp. 23±44, Aug. 26, 1991. U.S. Congress, Of®ce of Technology Assessment, Bioremediation for Marine Oil SpillsÐ Background Paper OTA-BP-O-70. U.S. Government Printing Of®ce, Washington DC, May 1991. Using Oil Spill Dispersants on the Sea. National Research Council, National Academy Press, Washington, DC, 1989.

190

EXERCISES

Vehicle Emissions Calvert, J. G., J. Heywood, R. F. Sawyer, and J. H. Seinfeld, Achieving acceptable air quality: Some re¯ections on controlling vehicle emissions, Science, 
, 37±44 (1993). Farruto, Robert J., Ronald M. Heck, and Barry K. Speronello, Environmental catalysis, Chem. Eng. New, p. 34, Sept. 27, 1992.

Coal Berkowitz, Norbert, An Introduction to Coal Technology, 2nd ed. Academic Press, San Diego, CA, 1994. Crawford, Don L., ed., Microbial Transformations of Low Rank Coals. CRC Press, Boca Raton, FL, 1993. Lumpkin, Robert E., Recent progress in the direct liquefaction of coal, Science, , 873±877 (1988). Schobert, Harold H., Coal: The Energy Source of the Past and Future. American Chemical Society, Washington, DC, 1987. Also see the references given at the end of Chapter 2.

EXERCISES 6.1. A supertanker with a large hole in its hull is sinking in 50 ft of water in the Mediterranean near the Italian Riviera. The immediate principal concern is whether the tanker will break up and release all its cargo before the oil can be pumped out of the wreck. The Mediterranean is generally calm at this time of year, and there are no storms in the forecast. You are in charge of minimizing the damage to the beaches and wildlife at this expensive resort area. (a) How will you remove the oil from the wreck? (b) How will you minimize the damage from the oil spilling into the Mediterranean? (c) How will you protect the beaches from the oil. How effective will your approach be? (d) Predict the short- and long-term effects of this spill on marine life in the area. 6.2. Two major tanker spills of the same amounts of Kuwait crude oil have occurred, one in the middle of the North Atlantic, far from land, where there are frequent storms, and the other in the calm water of Long Island Sound, close to highly populated areas in New York and Connecticut. Compare these spill with regard to the following: (a) Ease and feasibility of cleanup by means of ¯oating booms to control the spread of the oil and ships to ``vacuum'' it up (b) Rate of natural dispersal of the crude oil

191

6. PETROLEUM, HYDROCARBONS, AND COAL

(c) Extent of the immediate toxic effects on marine life (d) Possible short- and long-term toxic effects to residents (human and other) in the area of the spill. 6.3. A brilliant geology student at your university proposed a new theory for the formation of crude oil and predicted that there is a huge deposit under the school's football ®eld. Ten years after your graduation, preliminary drilling con®rmed the student's prediction. In spite of the pleas by the football coach and threats of bodily harm to the president by the football team, the university administration decides to proceed with drilling a well on the 50 yard line. As a prominent graduate from your university you are asked to outline the possible health and other hazards of this operation (drilling, pumping, and transporting) so that proper precautions could be taken to minimize the health and other hazards to students, staff, and faculty. Give your recommendations and discuss the scienti®c bases for them. 6.4. What are the most likely ®rst steps in the air oxidation of an ole®n present in oil spilled in the environment? Use the following generic formula for an ole®n in your proposed reactions. RCH2 CH ˆ CHR0 6.5. Predict the fate of each of the following compounds if introduced into the ocean as part of an oil spill. If the compound reacts chemically or is degrade by microorganisms under these conditions, give the equations(s) for the reaction in the environment. (a) Styrene (b) n-Butane (c) Benzo[a]pyrene (d) Asphalt (e) Kerosene (f) n-Propylbenzene 6.6. Write the chemical reactions for the initial steps in the combustion of isooctane (2,2,4-trimethylpentane) in the internal combustion engine. 6.7. Why can't an internal combustion engine be ``tuned'' (adjusted) to prevent it from emitting hydrocarbons, CO and NOx ? 6.8. The catalytic converter of present-day automobiles removes hydrocarbons (HC), CO, and NOx from emissions by both oxidative and reductive processes. (a) Brie¯y explain how oxidation and reduction of these compounds proceed in the same device. (b) Write balanced chemical equations for both the oxidation and reduction processes.

192

EXERCISES

(c) Why do you smell the emission of hydrocarbons from many cars equipped with functioning catalytic converters when their engines are ®rst started? 6.9. The addition of catalytic converters to the tailpipes of automobiles has resulted in a 10-fold or greater decrease in the emissions from new automobiles over the past 25 years. Give reasons for the much smaller decrease in the amounts of these gases in the atmospheres of urban areas.

7 SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

7.1 INTRODUCTION Soaps, surfactants and polymers are discussed together, following the discussion of petroleum, because most of the polymers and the surfactants in detergents are made mainly from chemicals derived from petroleum. Natural fats and oils are also used in the manufacture of surfactants (Figure 7-1). Soaps and surfactants contain segments of linear or lightly branched hydrocarbon chains that are, in the main, broken down to acetate up on metabolism by microorganisms in the environment. The biodegradation of petroleum occurs by the same pathway once a terminal carbon has been oxidized to a carboxyl grouping. The rate of degradation by other environmental reagents such as sunlight, oxygen, or water is much slower than that of microbial degradation. 193

194

7.1 INTRODUCTION

Principal Household Applications

Basic Starting Materials

Surfactants

Raw Materials

Benzene

Linear alkylbenzene

Linear alkylbenzene sulfonates

Heavy-duty laundry powders Light-duty liquid dish detergents Heavy-duty laundry liquids Specialty cleansers

Secondary alkane sulfonates

Light-duty liquid dish detergents

α-Olefin sulfonates

Liquid hand soap Light-duty liquid dish detergents Shampoos

Fatty amine oxides

Light-duty liquid dish detergents Shampoos Specialty cleansers

α-Sulfomethyl esters

Heavy-duty laundry powders

n-Paraffins

Linear αolefins

Fatty acids

Natural fats & oils

Fatty alkanolamides

Light-duty liquid dish detergents Shampoos

Alkyl polyglucosides

Light-duty liquid dish detergents

Alkyl glyceryl ether sufonates Detergentrange linear primary alcohols

Ethylene

Ethylene oxide

Linear alcohol ethoxylates

Alcohol sulfates

Toilet soaps Shampoos

Shampoos Heavy-duty laundry powders

Alcohol ether sulfates

Light-duty liquid dish detergents Heavy-duty laundry powders Heavy-duty laundry liquids Shampoos

Linear alcohol ethoxylates

Heavy-duty laundry liquids Heavy-duty laundry powders Specialty cleansers

FIGURE 7-1 Surfactants for household detergents: petrochemical raw materials and uses. Redrawn from ``Soaps and Detergents,'' Susan Ainsworth, Chem. Eng. News, Jan. 24, 1994. Used by permission of SRI Consulting. Also see color insert.

195

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

7.2 SOAPS AND SYNTHETIC SURFACTANTS Soaps and synthetic surfactants have similar structures, and their mechanisms of cleansing are similar. Both contain a hydrophobic portion (usually a hydrocarbon chain) to which a hydrophilic (polar) group is attached. Such materials are surface active: that is, they concentrate at the surface of an aqueous solution or form aggregates called micelles (Figure 7-2) within the solution. Surface-active materials lower the surface tension of the water so that the water better penetrates the surface and interstices of the object being cleaned. If the binding of the micelles of soap or synthetic surfactant to the substance being cleaned is greater than the binding of the soiling agent, the latter will then be transferred into the micelles upon agitation. Oils and greases will also be adsorbed by the hydrophobic end of the surface-active agent. The soiling agent can be washed away because the af®nity of the polar group of the surfactant for water keeps the micelle±dirt complex suspended in the water. The foam covering many otherwise scenic rivers and streams was a source of much public concern for many years. This environmental problem was caused by slowly degrading synthetic surfactants and was probably the ®rst modern environmental problem to be solved as a result of public opinion.

− −

−

−

−

−

−

−

− −

−

FIGURE 7-2 A Simpli®ed two-dimensional representation of a three-dimensional micelle. The hydrophobic hydrocarbon chains associate in the center of the micelle. Nonpolar substances associate with the hydrocarbon chains of the micelle, become solubilized, and are removed from the fabric.

196

7.2 SOAPS AND SYNTHETIC SURFACTANTS

Some indication of the nature of the problem was apparent as early as 1947 when the aeration tanks at the sewage disposal plant at Mount Penn, Pennsylvania, were inundated with suds. This spectacular effect was the result of a promotional campaign during which free samples of a new detergent had been distributed at local stores. Everyone used the new product at about the same time, but unfortunately the microorganisms residing at the disposal plant metabolized the synthetic surfactant in this detergent very slowly. Despite this early warning, slowly degrading surfactants were manufactured up to 1965 before the detergent industry responded to public pressure and voluntarily switched to the manufacture of surfactants that degrade more rapidly in the environment.

7.2.1 Soaps Soaps are prepared by the saponi®cation (base hydrolysis) of animal or vegetable fats as shown in reaction (7-1) (note, however, that the R groups are usually different). Hydrolysis converts the triglycerides in the fats to the sodium salts of carboxylic acids (soaps) and glycerol. The carboxylate group is the polar, water-soluble end of the soap. O RC O O

CH2

RC

CH + 3 NaOH

O

O RC

HO

CH2

O 3 RCO Na

+ HO

CH

…7-1†

Soap O

CH2

HO

CH2

Glycerol

The sodium salt of stearic acid, CH3 …CH2 †16 CO2 H, is the major product released upon hydrolysis of animal fat, while the sodium salt of oleic acid, CH3 …CH2 †7 CH ˆ CH…CH2 †7 CO2 H, is the main product from the hydrolysis of olive oil. Hydrolysis of palm oil yields approximately equal amounts of the salts of oleic acid and palmitic acid, CH3 …CH2 †14 CO2 H. These naturally occurring fatty acids contain linear hydrocarbon chains, which are synthesized biochemically from the acetate ion (CH3 CO2 ). They are also readily degraded back to acetate by microorganisms in the environment. Since long-chain (``fatty'') acids occur naturally, it is not surprising to ®nd some foam and suds at waterfalls, the surf at the beach, and other places of turbulence in streams, rivers, and oceans owing to the presence of natural soaps in the water. The main disadvantage of the use of salts of carboxylic acids as cleansing agents is the insoluble precipitates that form with Ca2‡ and Mg2‡ , which when

197

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

present in water make it hard. This curdy, gray precipitate leaves a deposit on clothes or ``ring'' around collars or bathtubs. Not only are the deposits undesirable, but greater amounts of soap must be used to make up for that lost by precipitation. Another disadvantage of soaps is that they are salts of weak acids that protonate in mildly acidic solutions. The polarity of the ``head'' of the detergent decreases when protonated and, as a consequence, the product's effectiveness at solubilizing oils and greases is diminished.

7.2.2 Detergents Detergents are a mixture of synthetic surfactants, builders, bleaches, enzymes, and other materials designed to enhance the speci®c cleaning power of this mixture. Millions of pounds of these materials are produced in the United States each year (Table 7-1). The main advantage of synthetic surfactants over soaps is that the former do not precipitate in hard water. Since, however the cleansing power of synthetic surfactants is also decreased markedly by Ca2‡ and Mg2‡ , it is necessary to add builders that enhance the cleansing action of synthetics by inactivating the Ca2‡ and Mg2‡ in hard water. The builders are polycarboxylic acids, silicates, zeolites (inorganic aluminosilicates), or polyphosphates (e.g., Na5 P3 O10 ; Section 10.5), which bind Ca2‡ and Mg2‡ thus preventing them from binding to the surfactant. Polyphosphates, which were used extensively as builders in the 1970s, were replaced in large part by zeolites because it was believed that phosphate from polyphosphates initiated algal blooms on lakes (Section 9.1.2), with the resulting eutrophication. Since the phosphate in detergents is easily removed by treatment with Fe3‡ at sewage disposal plants, a process that has been in use in Sweden for many years, it may have been premature to ban the use of polyphosphates. It should also be noted

TABLE 7-1 U.S. Detergent Chemical Use in 1996

Use

Amount …lb  106 †

Builders Surfactants Bleaches, brighteners, and enzymes Fragrances and softeners Other

3805 2000a 190 128 260

a

Surfactant use in 2001 projected to be 2400 106 lb. Source: E. M. Kirschner, Chem. Eng. News, p. 39, Jan. 26, 1998.

198

7.2 SOAPS AND SYNTHETIC SURFACTANTS

that detergents account for only 20±25% of the phosphate in lakes and rivers, while the bulk of the remainder comes from fertilizer and animal waste runoff from farms. Consequently, the phosphates in detergents are not the main cause of lake eutrophication. In accordance with the view that phosphates have a minor role in lake eutrophication, these compounds have been classi®ed as ecologically acceptable for use in home laundry detergents in Europe. Currently 25% of the home laundry detergents sold in Europe contain phosphates. It is reported that zeolites are not as effective as polyphosphates in enhancing the cleansing power of surfactants and that they have environmental problems as well. Studies suggest that zeolites promote surface algal blooms in the Adriatic Sea. In natural waters they bind naturally occurring humic acids (Section 9.5.7) to form particles that ¯oat. Microorganisms that bind to these particles grow and produce a foul-smelling algal bloom.

7.2.3 Surfactants 7.2.3.1 The General Nature of Surfactants

It has been possible to synthesize a wide variety of surfactants by varying the structure of both the polar and nonpolar ends of the molecule. The polar end of the linear alkylsulfonates is the anionic sulfonate group RSO3 . The linear alkylsulfonates [see later: reaction (7-7)] and alcohol sulfate CH3 j ‰CH3 …CH2 †n CHOSO3 Na‡ and the related alcohol ether sulfates RO…CH2 CH2 CH2 †n CH2 CH2 OSO3 Na‡ are the major laundry surfactants used in the United States (Table 7-2). The nonionic surfactants, alcohol ethoxylates [RO…CH2 CH2 †n CH2 CH2 OH], and alkylphenol ethoxylates [see later: reaction (7-11)], which have alcohol groups as the polar entity, are also produced in large amounts (Table 7-2). Smaller amounts of cationic surfactants [CH3 …CH2 †n CH2 N…CH3 †3 Cl ] are also manufactured. These are not as ef®cient as the anionic and nonionic cleaning agents but are used as germicides and fabric softeners. 7.2.3.2 Synthesis of Linear Alkylsulfonates (LAS)

Alkyl benzene sulfonates (ABS), the original slowly degrading surfactants, and linear alkylsulfonates are prepared by similar procedures. The alkyl chain in both is prepared by the oligomerization (formation of short polymers) of

199

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

TABLE 7-2 Laundry Surfactant Use in the United States in 1991 Surfactant Linear alkylsulfonates Alcohol sulfates Alcohol ether sulfates Alcohol ethoxylates and alkylphenol ethoxylates Other anionics


 Amounts lb  106

Percent

740 220 260 390 200

40 12 14 21 11

Source: Modi®ed from A. M. Thayer, Chem. Eng. News, p. 33, Jan. 25, 1993.

propene (propylene), but with the ABS derivatives a branched oligomer is formed in the following acid-catalyzed process: CH3

CH3 CH3CH CH2 + H

CH3CH

(CH3)2CHCH2CH

CH3

CH3 2CH3CH CH2

CH3CH CH2

…7-2†

(CH3)2CH(CH2CH)2CH2CH CH3

(CH3)2CH(CH2CH)2CHCH CH2 + H

It is not possible to synthesize linear hydrocarbon molecules by the straightforward acid-catalyzed oligomerization of ole®ns because the more substituted secondary carbocation is formed, with the formation of a branched chain hydrocarbon as shown in reaction (7-2). The branched-chain oligomers were used because they were readily prepared in acid-catalyzed reactions. Linear hydrocarbons can be synthesized or separated from petroleum. They can be synthesized from ole®ns by use of catalysts such as triethylaluminum to give either alkanes or alkenes. In the Alfol process, linear alcohols are formed by the air oxidation and subsequent hydrolysis of the oligomers formed initially [reactions (7-3) and (7-4)]. Ole®ns can be formed by pyrolysis of the trialkylaluminum adduct in the presence of ethylene in reaction (7-5). CH2CH3 CH3CH2 Al CH2CH3 + n CH2 CH2 Al (CH2CH2)nCH2CH3 + H3O

O2

Al

(CH2CH2)nCH2CH3

Al O(CH2CH2)nCH2CH3

CH3CH2(CH2CH2)nOH + Al(OH)3

…7-3†

…7-4†

,,

7.2 SOAPS AND SYNTHETIC SURFACTANTS

Al (CH2CH2)nCH2CH3

C H2

CH2

∆

…7-5† CH3CH2(CH2CH2)n-1CH CH2 + Al(CH2CH3)3

Urea crystallizes in a unique fashion from hydrocarbon solutions, and this is the basis of a method of separating linear and branched hydrocarbons in petroleum fractions. Linear hydrocarbons may separate from the branched-chain kind in petroleum fractions by encapsulation in the urea crystals. The urea crystallizes as helices, with the linear hydrocarbons encased in the central channel of the tubes formed by these helices. Branched-chain hydrocarbons do not ®t into the 5-AÊ-diameter tube, so the linear hydrocarbons can be separated by merely ®ltering out the urea crystals. ``Lightly branched'' hydrocarbons with more than 10 carbon atoms will also form urea inclusion compounds and these are also present in the mixture of ``linear'' hydrocarbons separated by this procedure. The use of molecular sieves has provided a cheaper means for the separation of linear and branched hydrocarbons than the use of urea. Molecular sieves are semipermeable zeolites that have a channel structure similar to that of urea when it is crystallized from hydrocarbons. The molecular sieves with a diameter of 5 AÊ (0.5 nm) are used to selectively screen linear hydrocarbons from petroleum. Virtually the same procedures are used to complete the synthesis of both the ABS and linear alkylsulfonate detergents. The propene or other ole®n oligomer is attached to benzene in an acid-catalyzed Friedel±Crafts reaction (7-6), the alkylated benzene is sulfonated with sulfur trioxide, and then, in reaction (7-7), the sulfonic acid product is neutralized with NaOH to generate the anionic surfactant. CH3 R′CH

CH2

HF

CH3 R′HC

R′HC

…7-6†

CH3 1. SO 3 2. NaOH

R′HC

SO3 Na

…7-7†

7.2.3.3 Synthesis of Nonionic Alcohol Ethoxylates

The alcohol and alkylphenol ethoxylates, the largest group of nonionic detergents currently in use, are prepared from the anion of the alcohol or alkylphenol and ethylene oxide. Reactions (7-8)±(7-11) (n ˆ 5±10) outline the synthesis of the nonylphenol ethoxylate, one of the major nonionic detergents manufactured in the United States.

201

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

C9H19

OH

OH

C9H19

O

+

O + H2O

C9H19

O

OCH2CH2O

C9H19

…7-8†

…7-9†

Ethylene oxide

C9H19

OCH2CH2O

+ n

O

…7-10† O(CH2CH2)nCH2CH2O

C9H19

C9H19

O(CH2CH2)nCH2CH2O

H

…7-11† C9H19

O(CH2CH2)nCH2CH2OH

7.2.4 Microbial Metabolism of Hydrocarbons, Soaps, and Synthetic Surfactants Microorganisms can utilize the energy of oxidation released by some hydrocarbons, soaps, and surfactants as well as some of the organic fragments released during their growth. The metabolism of these compounds is affected by enzymesÐhigh molecular weight proteins that catalyze a broad range of chemical transformations in living systems. Enzymes are characterized by their extreme catalytic ef®ciency (the catalyzed reactions typically proceed about 109 times as fast as the uncatalyzed reaction) and speci®city. (There is usually a speci®c enzyme for each chemical transformation that takes place in a cell.) Many enzymes require a small, nonprotein prosthetic group, called a coenzyme, for catalytic activity. Coenzymes are bound to the enzyme during the course of the reaction, and sometimes they combine with one or more of the reacting chemical species. Fatty acids (including protonated soaps) occur widely in biological systems and are therefore readily degraded by microorganisms in enzyme-catalyzed reactions. Linear hydrocarbons and linear detergents are similar in structure to soaps, and these are degraded in the same or similar pathways. O RCH2CH2CO2H + CoASH

RCH2CH2CSCoA

…7-12†

,

7.2 SOAPS AND SYNTHETIC SURFACTANTS

O

O

RCH2CH2CSCoA + FAD

RCH

OH

O CHCSCoA + H2O

RCH OH

O

O

RCHCH2CSCoA

O

O

RCHCH2CSCoA + NAD

CHCSCoA + FADH2

O

RCCH2CSCoA + NADH + H

O

O

O

RCCH 2CSCoA + H2O

RCOH + CH3CSCoA

…7-13† …7-14† …7-15† …7-16†

The steps in the oxidative metabolism of fatty acids are outlined in reactions (7-12)±(7-16). Each of these reactions is catalyzed by an enzyme even though the enzyme is not speci®ed in the reaction. Coenzyme A (CoASH) is a complex structure that contains a thiol group (ÐSH) as the reactive center. The acetyl coenzyme A [CH3 C…O†SCoA] produced in reaction (7-16) may be used by the microorganism for the synthesis of the speci®c fatty acids needed for growth by a pathway that is essentially the reverse of the one shown here. Alternatively, the acetyl CoA may be oxidatively degraded to carbon dioxide and water to provide the energy needed to drive microbial metabolic processes. Flavin adenine dinucleotide (FAD) and nicotinamide adenine dinucleotide (NAD‡ ) are the oxidized forms of hydrogen transfer coenzymes, while FADH2 and NADH are the respective reduced forms. Originally it was believed that branching in the alkyl chain of alkylbenzene sulfonate (ABS) detergents impeded speci®c steps in reactions (7-12)±(7-16) and that this was the reason for their slow environmental degradation. It was proposed that the branched hydroxyester reaction formed in (7-17) would not be oxidized further to the keto derivative [see reaction (7-15)] and biodegradation would be halted at this roadblock. However, it has been found that microorganisms are able to get around these simple barriers either by oxidatively removing the methyl groups or by cleaving off propionyl CoA [CH3 CH2 C…O†SCoA] in place of acetyl CoA. Chain branching merely slows the degradative process. O RC

CHCSCoA + H2O

CH3

OH

O

RCCH2CSCoA

…7-17†

CH3

The biodegradation of surfactants has been studied in considerable detail, but their structural diversity, even within speci®c types, makes it dif®cult to

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

203

formulate guidelines for biodegradation based on structure. These studies are further confused by the need to ``acclimate'' the bacteria population with the surfactant to ensure that consistent results are obtained. The need for acclimation suggests that all the members of the population are not able to metabolize the surfactant and acclimation promotes the growth of strains of microorganisms that are able to degrade it. The following guidelines have been developed to facilitate understanding of the microbial degradation of ABS and LAS detergents. 1. Highly branched ABS detergents degrade slowly in part because the alternative pathways required to cleave the side chain methyl groups proceed more slowly than the route shown in reactions (7-12)±(7-16). 2. The ease of cleavage of the surfactant increases, the further the polar sulfate or sulfonate grouping is from the alkyl terminus of the chain. Consequently, surfactants with branched chains that are shorter than those with linear chains containing the same number of carbon atoms degrade more slowly. This rule may be related to the ease of binding of the surfactant to a degradative enzyme if the site for binding its polar group is in a hydrophilic region of the enzyme and the site for binding its hydrophobic end is in a hydrophobic region of the enzyme. 3. The rate of degradation of surfactants is slower in concentrated solutions than in dilute solutions. This ®nding suggests that minor constituents of the surfactant mixture inhibit the microbial degradative enzymes. Their concentrations are not high enough in dilute solutions to inhibit all the microbial enzyme present. These guidelines also apply to the alkyl substituent of the alkyl- and alkylphenol ethoxylates. The alkyl chain will degrade slowly if it is highly branched, and then the ethoxylate grouping will degrade ®rst. The rate of degradation of the alkyl chain decreases as the number of ethoxylate groups increases. For example, the extent of degradation of the ethoxylate chain of an alkylphenol ethoxylate decreases as the number of ethoxylate groupings increase from 5 to 20. This decrease may re¯ect the increased dif®culty of transport of the more hydrophilic detergent (with more ethoxylate groupings) through the hydrophobic cell membrane of microorganisms. The alkylphenol ethoxylates degrade more slowly than the alcohol ethoxylates. In some cases it has been possible to isolate what appear to be intermediates in the degradation of the alkylphenol ethoxylates in which one or two ethoxylate groupings remain attached to the alkylphenol. These compounds have little surfactant action or solubility and precipitate with the other sludge at the waste disposal plant (Section 11.5.2). Their anaerobic (nonoxygenic) degradation product, nonylphenol, has been found in sewage sludge [see reaction (7-18)].

204

7.2 SOAPS AND SYNTHETIC SURFACTANTS

H

OCH2CH2OCH2CH2OH

C9H19

OH

C9H19

…7-18† Nonylphenol [H] = microbial degradation under reducing conditions

Nonylphenol is toxic to ®sh and other marine life, and it may be an environmental hazard when it is leached from sewage sludge that is dumped on land or in the ocean. It is also has estrogenic hormonal activity in mammals (Section 8.5.1). It is not clear whether the nonylphenol released by the degradation of nonionic surfactants is present in suf®cient quantities in the environment to cause estrogenic effects. While the biochemical pathway for the degradation of ethoxylate surfactants has not been determined, some insight into the mechanism can be obtained from studies on the degradation of glycols and simple ethoxylate oligomers shown in reaction (7-19). HO O

HO ROCH2CH2OH

O

ROCHCH2OH

O

HO O

ROCHCH

O

ROCHCOH O

O ROCH2OH + CO2

O

H 2O

ROCH

ROH + HCOH

…7-19†

R = HOCH2CH2OCH2CH 2O– , where [O] indicates oxidation.

The microbial breakdown of detergents and petroleum requires the terminal oxidation of the hydrocarbon chain to a carboxylic acid group to initiate the boxidation procedure outlined in reactions (7-12)±(7-16). This terminal oxidation is a well-documented process, and in some instances it has been established that the corresponding alcohol and aldehyde are reaction intermediates. Molecular oxygen is the oxidizing agent, and the oxygen is activated by binding to the iron-containing enzyme cytochrome P-450. The reaction follows the following sequence: RCH2CH2CH3

O

RCH2CH2CH2OH

O

RCH2CH2CO2H

O

…7-20†

R2CO2H + CH3CO2H

As discussed in Section 6.4, these reactions are carried out in microorganisms, but are slow, especially with high molecular weight materials that do not readily pass through the microbial cell wall. The microbial oxidation of the cyclic hydrocarbons and aromatic compounds present in detergents and petroleum is also catalyzed by the enzyme

205

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

cytochrome P-450 in microorganisms. It has been established in some cases that arene oxide intermediates are formed, as in the following reaction sequence for the oxidation of benzene. OH H OH H

cytochrome

O

P-450

Arene oxide

OH

OH Catechol

…7-21† CH3CO2H + O O HOC

O

CO2H

O

CO2H

CCH2CO2H

CO2H

CO2H

CO2H

O

The microbial oxidation of the more highly condensed aromatics such as naphthalene or of the alkyl-substituted benzenes proceeds via salicylic acid, which is then oxidized to catechol in accordance with reaction (7-22) and ®nally to oxaloacetate.

CO2H

OH

or OH Salicylic acid

OH

…7-22†

Catechol

CH3

The sulfate esters in alcohol sulfates are readily hydrolyzed by microbial sulfatase enzymes. Sulfonates present in the surfactants are subject to rapid oxidative elimination by a variety of aquatic bacteria: OH RCH2SO3

O

H R

SO3

O

R

…7-23†

RCHO + HSO3

RCHSO3

OH OH SO3

OH R

OH + HSO3

…7-24†

206

7.2 SOAPS AND SYNTHETIC SURFACTANTS

Therefore, these sulfonate groups do not slow the environmental degradation of the alcohol sulfates. The bisul®te formed is rapidly oxidized to bisulfate by microorganisms.

7.2.5 Environmental Effects of Biodegradable Organic Compounds: Biological Oxygen Demand The presence of biodegradable organic compounds in lakes and rivers can result in an environmental problem. Oxygen is required for the microbial degradation of these compounds, and relatively small quantities of organic material can deplete the supply of dissolved oxygen. The amount of oxygen consumed in the microbial degradation of organic compounds can be estimated if the crude assumptions are made that the organic compounds are pure carbon and that they are all converted to carbon dioxide. C ‡ O2 ! CO2

…7-25†

From reaction (7-25) and the ratio of the molecular weight of oxygen to the atomic weight of carbon, it can be seen that 32=12, or about 2.7 g of oxygen, is required to oxidize 1 g of carbon. Since water can dissolve only about 10 ppm of oxygen, this means that in the absence of further dissolution of atmospheric oxygen, only 4 ppm of carbon compounds can deplete all the dissolved oxygen in a body of water. This calculation is an oversimpli®cation because microbial oxidation does not proceed instantly and the oxygen is always being replenished. However, the oxygen near the bottom of deep lakes can be depleted by dissolved organics because of the slow rate of oxygen transport to these low levels (Chapter 9). Fish have dif®culty breathing when the oxygen level drops to 5 ppm (one-half the maximum level). Biological oxygen demand (BOD), a measure of the biodegradable organic material in water, is determined by the amount of oxygen required for the microbial oxidation of the dissolved organic content of a water sample. The analysis measures the amount of dissolved oxygen lost from a water sample kept in a sealed container at 28C over a 5-day period. Chemical oxygen demand (COD) is another measure of dissolved organic compounds. It is determined by measuring the equivalents of acidic permanganate or dichromate necessary for the oxidation of organic constituents. Neither BOD nor COD measures the total oxidizable carbon (TOC) content. Total oxidizable carbon is measured by the amount of CO2 formed upon combustion after the water and the carbonate in the sample have been removed. Biodegradable and chemically degradable compounds reduce the oxygen level in lakes and rivers. However, the major sources of dissolved organics in lakes and rivers are the ef¯uent from sewage disposal plants, manure from animal feed lots, industrial wastes, and decomposing plants and algae.

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

207

7.3 POLYMERS Polymers are macromolecules, that is, molecules containing many atoms that are of very large size and high molecular weight (ranging from 10 KDa to over 100 kDa). They are made up of a small number of repeating groups. Many macromolecules are components of living systems; examples are proteins, which are polymers of amino acids, and starch and cellulose, which are polymers of cyclic polyhydroxy compounds (sugars). Since biological polymers are built up in living systems, they can typically be broken down by these systems (i.e., they are biodegradable). Biodegradable substances will not cause long-term environmental problems, although the decomposition of large amounts of such materials can be a problem in the short term through their effect on the BOD. In aqueous solution, their degradation will contribute to the biological oxygen demand and use up the dissolved oxygen (see Section 7.2.5). The latex obtained from the sap of rubber trees is apparently an exception to the rule that naturally occurring polymers are biodegradable. The latex is modi®ed by cross-linking and other processes during its formulation into tires, gloves, and other products. These chemical processes increase the strength and durability of the material and also its resistance to biodegradation. Synthetic polymers are made up of a great number of simple units (monomers) joined together in a regular fashion. Some examples are given in Figures 7-3 and 7-4. Many plastic items are not formulated from the polymeric material alone. They may contain lower molecular weight compounds called plasticizers that increase their ¯ow and processibility. Polychlorinated biphenyls (PCBs) were formerly used for this purpose, as mentioned in Chapter 8. Esters of phthalic acid are other examples of plasticizers. Fillers, such as wood ¯our, cellulose, starch, ground mica, asbestos, or glass ®ber, are often added to increase the strength of the plastic or to provide bulk at low cost. Heavy metal compounds, including those of tin, cadmium and lead (Sections 10.6.7 and 10.6.10), may be present as plasticizers or to confer resistance to degradation. Plasticizers may be leached or evaporated from polymeric materials in use, while both plasticizers and ®llers may contribute to problems of environmental disposal and degradation. The release of PCBs upon incineration of chlorinated polymers is referred to in Chapter 8. Fillers may be inert, but if released as dust during incineration of wastes, they can contribute to atmospheric particulate material. Asbestos particles are health hazards, in view of the known connection between asbestos dust and lung cancer. In August 2000 an independent panel appointed by the U.S. National Toxicology Program reported ``serious concern'' that when vinyl polymers are used, the ``exposure to intensive medical procedures may have adverse effects on the reproductive tract of male infants.'' The basis for this concern is that di(2-ethylhexyl)phthalate (DEHP) may be leached from vinyl tubing by

208

7.3 POLYMERS

Monomer(s)

Polymer

Repeat unit

Polyethylene

CH2CH2

H2C

Polypropylene

CHCH2

CH3HC

CH2 CH2

CH3 CHCH2 CH CH2

Polystyrene

Poly(methyl methacrylate)

OCH3

OCH3

C

C

O

CH2C

O

H2C

CCH3

H2C

CHCl

CH3 CH2CH

Poly(vinyl chloride)

Cl O

Nylon 66

O

O

C(CH2)4CNH(CH2) 6NH

O

HOC(CH2)4COH and NH2(CH2)6NH2

Poly(ethylene terephthalate) (PET)

O

O

HOCH2CH2OH

C

COCH2CH2O

O HOC

and

O COH

FIGURE 7-3 Some typical nonbiodegradable polymers and the monomers from which they are formed.

¯uid running through it to an infant with a medical problem. The ``serious concern'' was directed to the use of vinyl polymers that contained DEHP (Figure 7-5) as the plasticizer. Six other commonly used phthalate ester plasticizers were rated as generating only ``minimal'' or ``negligible'' concern. The panel also raised the ``concern'' that the ``exposures of pregnant women to

209

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

Repeat unit

Polymer

Monomer(s) CH3

CH3 C

Poly(vinyl acetate)

C

O

O

O

O H2C

CH2CH

CH

OH Poly(vinyl alcohol)

CH2CH

Poly(ethylene oxide)

CH2CH2O

O H2C

CH2

O Polyglycolate

HOCH2CO2H

OCH2C O

HOCHCO2H

OCHC

Polylactate

CH3

CH 3 O Poly(β-hydroxybutyrate)

HOCHCH2CO2H

OCHCH2C

CH3

CH3 O Poly(β-hydroxyvalerate)

HOCHCH2CO2H

OCHCH2C

CH2CH3

CH2CH3

O

O Polycaprolactone O Poly(ester urethane)

O

O(CH2)5C O

O

O

NHCHCOCH2CH2OCCHNHCNHCH2CH2NHC R

R

O

C

NCH2CH2N C O

and

O

O

NH2CHCOCH2CH2OCCHNH2 R H3C Poly(cis-1,4-isoprene) H2C

R H3C

CH2-

H2C

CH2

FIGURE 7-4 Some typical polymers that are biodegradable under aerobic conditions only and the monomers from which they are formed. Note that a poly(vinyl alcohol) monomer is not formed by the polymerization of the vinyl alcohol but rather by hydrolysis of poly(vinyl acetate).

210

7.3 POLYMERS

CH2CH3 COOCH2CH(CH2)3CH3 COOCH2CH(CH2)3CH3 CH2CH3 FIGURE 7-5 The structure of the phthalic acid plasticizer di(2-ethylhexyl)phthalate.

DEHP might affect development of their offspring.'' The concern arose from rodent studies in which juvenile rats that ingested DEHP had lower testicular weight, testicle degeneration, and reduced sperm counts in comparison to controls. From these results, the possibility was raised that DEHP might be leached from vinyl surgical tubing by ¯uid running through it to infants with serious medical problems. In addition the report led many toy manufacturers to stop making toys with plastics that contained phthalate plasticizers. While there are few expensive or non toxic plasticizers that can replace phthalates in vinyl polymers, there are plastics that can replace vinyl in medical devices. DEHP is also a potential carcinogen. Phthalates are abundant in the environment because they are used extensively (10  109 lbs produced worldwide in 1999) and because they are degraded at a moderate rate by microorganisms that use a variation on the oxidative pathway illustrated in reaction (7-24). The bulk of the monomers used in polymer synthesis are synthesized directly or indirectly from petroleum. Therefore, our present dependence on plastic materials is ultimately a dependence on sources of crude oil.

7.3.1 Polymer Synthesis Polymers may be formed from monomers in chain reaction or step reaction polymerization. The chain reaction process is illustrated by the free-radical polymerization of ethylene or its derivatives. The speci®c example of the polymerization of acrylonitrile to Orlon is given in reactions (7-26)±(7-30). ROOR

RO

+ H2C

…7-26†

2RO

CH

ROCH2CH

CN

CN

…7-27†

211

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

ROCH2CH

+ H2C

CN

CN

ROCH2CHCH2CH

CN

CN

CN

…7-29† CHCH2(CHCH2)nCHCH2OR

ROCH2CH(CH2CH)nCH2CH CN

2 ROCH2CH(CH2CH)nCH2CH CN

CN

…7-28†

CN

combination

2 ROCH2CH(CH2CH)nCH2CH CN

CH

CN

CN

CN

CN

CN

disproportionation

CN

…7-30† CH + CH2CH2(CHCH2)nCHCH2OR

ROCH2CH(CH 2CH)nCH CN

CN

CN

CN

CN

CN

In free-radical polymerizations, a small amount of initiator, such as a peroxide, is added to the monomer to start the polymerization. The initiator decomposes to form radicals (7-26), which add to the monomer in the chain-initiating step (7-27). Further addition of monomer takes place in the chain-propagating step (7-28). Polymer growth stops in the chain-terminating steps, which require the reaction of two radicals such as the combination and disproportionation reactions shown in (7-29) and (7-30). Ionic processes may also be involved in chain reaction polymerization. Cationic polymerization of vinyl monomers is initiated by acids. The synthesis of propene oligomers from propene by this process has already been discussed (Section 7.2.3.2). Anionic polymerization is often initiated by strong bases such as butyllithium (CH3 CH2 CH2 CH2 Li‡ ). In these chain reaction polymerization processes, the molecular weight of the ®nal polymer is dependent on the maintenance of the active species, be it the radical, cation, or anion formed initially. In step reaction polymerization, monomers and oligomers react to form polymers. The formation of a nylon illustrates this process: O

O

O

HOC(CH2)4COH + NH2(CH2)6NH2

H2O

O

HOC(CH2)4CNH(CH2)6NH2 O

NH2(CH2)6NH H2O

O

NH2 (CH2)6 NHC(CH2)4CNH(CH2)6NH2 O

continued addition of monomers and reaction between oligomers already formed

O

C(CH2)4CNH(CH2)6NH a Nylon

n

…7-31†

212

7.3 POLYMERS

The polyester poly(ethylene terephthalate) (PET), (Dacron or Terylene) is prepared in a similar fashion from ethylene glycol and terephthalic acid (reaction 7-32). These step reaction polymerizations are examples of condensation polymerizations. A small molecule, water here, is eliminated in each step. Many of the biodegradable polymers are aliphatic polyesters prepared by step reaction condensation reactions as shown earlier (Figure 7-4). HOCH2CH2OH + HO2C

CO2H O

O

OCH2CH2OC

C

…7-32† n

PET

7.3.2 Paper Paper is composed mainly of cellulose, a polymer made up of b-glucose units linked through oxygen atoms. Paper is generally produced by the chemical removal of lignin, resins, and other components of wood to leave cellulose ®bers (pulp), which is compacted to produce the paper sheet. Mechanical grinding can also be used to facilitate the removal of the lignin, but this yields a lower quality paper. The kraft pulping process hydrolyzes the lignin with a sodium hydroxide±sodium sul®de solution, producing organic sulfur compounds and other organic material in what is called black liquor. This can be a considerable source of pollution, but most of it is treated and recycled for reuse of the reactants. The sul®te process, used for high-quality papers, uses calcium and magnesium sul®tes produced from SO2 and the corresponding carbonate. The pulp, especially from the kraft process, contains oxidized organic compounds that produce a brown color and must be bleached. Traditionally, this has required chlorine to produce the actual bleaching agent employed, chlorine dioxide (Section 11.5.1). Paper manufacturing thus has been a heavy user of chlorine and sodium hydroxide, and paper plants have often operated their own chloralkali plants with their associated environmental problems (Section 11.5.1). Recent practice is to replace the chlorine-based bleach with an alternative process that employs oxygen as the bleaching agent, Most paper products contain various additivesЮllers such as clay or titanium dioxide, resins to improve wet strength, sizings, coloring, and so on. These differ depending on the type of paper and add to the complications of paper recycling (Section 16.7.2).

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

213

7.3.3 The Fate of Polymers after Use About 108 million tons of plastics was produced in the world in 1996, with 24% of the production in the United States, 25% in western Europe, 9% in Japan, and 25% in the rest of Asia. In the same year western Europe discarded 19.3 million tons of plastic waste; 10% of this waste was recycled, 14% was used for energy, and the rest was placed in land®lls. In 1990 25 million tons of plastics was manufactured in the United States, while during the same time period 16 million tons was placed in land®lls (this does not include about 1.8 million tons of tires also placed in land®lls). Only about 0.4 million tons of the plastic was reused or recycled. Plastic material constitutes about 10% by weight and 20% by volume of the material in land®lls, with paper being the principal constituent at 32% by weight and by volume. As discussed in Section 16.2, relatively little decomposition takes place in land®lls, so very little of this plastic material disappears with time. The plastic that is not placed in land®lls, recycled, used for energy, or incinerated, is scattered either on land or in the sea. These materials, which have been designed to be strong and stable, persist for a long time. For example, it is estimated that the six-pack plastic strap made of high-density polyethylene has a lifetime of 450 years in the sea. It is estimated that 6 million tons of garbage is dropped in the oceans each year by boats. The amount of plastic material in this garbage has not been estimated, but it includes commercial ®shing nets, ®shing line, ropes, bags, lids, six-pack rings, disposable diapers, gloves, tampon applicators, bottles, plastic foam, and pellets to name a few. The principal concern associated with plastic materials scattered on land is one of aesthetics, not toxicity or harm to ecosystems. Plastic articles dumped in oceans are not aesthetically pleasing when they wash up on beaches, but of even greater importance is their danger to marine life. It has been estimated that plastics kill or injure tens of thousands sea birds, seals, sea lions, and sea otters each year, and hundreds of whales, porpoises, bottlenose dolphins, and sea turtles. A large portion of the reported fatalities are due to the entanglement of birds and mammals in the driftnets of commercial ®shing boats. These nets, up to 30 km long, entangle seals, bottlenose dolphins, porpoises, and birds. For example, the 4±6% annual decline in the population of the northern fur seal (20,000±40,000 seals), which live in the Bering Sea off Alaska, is attributed to entanglement in drift nets. Most of these drift nets are in use and cannot be classi®ed as a disposal problem, but free-¯oating drift nets, which have broken loose or have been discarded and continue to trap sea life, are an environmental problem. The most dramatic victims are whales that are unable to dive and feed because they are entangled in large piece of drift net. Dying, beached whales wrapped in drift nets have been found on both the east and west coasts of the United States.

214

7.3 POLYMERS

Other plastic items also endanger sea life. For example, seal pups play with plastic items ¯oating in the sea. If pups happen to stick their heads through plastic collars, as they grow the plastic will sever their neck arteries or strangle them. Of perhaps even greater danger is the ingestion of plastic items by some marine life. A ¯oating plastic bag can look like a tasty jelly®sh to a sea turtle. When turtles consume a lot of plastic it blocks their intestines, preventing them from assimilating food. Sea birds, which often mistake plastic pellets for ®sh eggs or other marine food, also suffer from intestinal blockage if they consume large quantities of plastic. The use of biodegradable polymers will help to reduce the level of plastic in the ocean, but extensive research will be necessary to develop polymers that not only are biodegradable but also have the strength and other desirable properties of the nonbiodegradable polymers in use today. Moreover, after such materials have been developed, the consumer will have to be convinced to purchase biodegradable products even though they will slowly degrade and therefore may have a shorter useful life than the corresponding nonbiodegradable product. 7.3.3.1 Biodegradable Polymers

A goal of the plastics industry is to design biodegradable polymers that can be substituted for materials that are dif®cult to collect and reuse. These include water-soluble polymers, polymers designed for use for ®shing or other marine applications that end up in the marine environment, and polymers employed with other materials such as coatings on cups, diapers, and sanitary products. Polymers that tend to be used only once such as six-pack plastic straps, plastic cutlery, and hospital waste should also be degradable. Microorganisms use degradable polymers for their growth, and thus the polymer will be converted to compounds that can be utilized in the natural cycle of life on earth. As noted already, these polymers will break down only where there is abundant molecular oxygen, so the designation ``biodegradable'' does not apply to the anaerobic environment in a land®ll.

7.3.4 Environmental Degradation of Polymers 7.3.4.1 Nonbiodegradable Polymers

Many hydrocarbon polymers have chemical reactivity similar to that of high boiling petroleum fractions and, as a consequence, these compounds are very persistent in the environment (Section 7.2.4). Until recently, the goal of the polymer chemist was to design a polymer that degrades very slowly in the environment. Each new polymer was tested extensively to be sure that it did not break down rapidly in its particular use. For example, a material designed

215

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

for use in vinyl siding for homes would be tested for its resistance to degradation by oxygen, water, and sunlight. Some products made from vinyl polymers appear to degrade in the environment, but this is mainly due to the loss of their phthalate ester plasticizer, which results in a change of the mechanical properties of the polymer. They vinyl products become brittle and crack, but the actual degradation of the the polymer proceeds more slowly. 7.3.4.2 Photooxidation

Polymers will be degraded if they absorb sunlight at wavelengths greater than that of the radiation that is not absorbed by stratospheric ozone (290 nm: see Section 5.2.3). Since many polymers do not have functionality that results in light absorption at wavelengths greater than 290 nm, direct photolysis is not usually a major degradative pathway. Indirect photochemical processes, such as oxidation by photochemically generated singlet oxygen (Sections 5.2.2 and 6.4) can also result in polymer degradation. The peroxides formed by polymer processing may trigger photochemical polymer degradation. Mechanical shearing of polymers during processing results in radical formation as a result of chain breaking [reaction (7-33)], and these radicals react with molecular oxygen to form hydroperoxides, as shown in reaction (7-34) and (7-35). mechanical shearing

Rƒƒƒƒƒƒƒƒƒƒƒƒƒ! 2R. R. ‡ O ! ROO.

…7-34†

ROO. ‡ RH ! ROOH ‡ R.

…7-35†

R

2

…7-33†

Hydroperoxides absorb light at wavelengths greater than 290 nm and are cleaved to hydroxyl radicals and alkoxy radicals with a quantum yield close to one, according to reaction (7-36). ROOH ƒƒƒƒ! RO. ‡ . OH hn

The radicals react further as follows to form alcohols: RO. ‡ RH ! ROH ‡ R.

…7-36†

…7-37†

Alternatively, hydroperoxides cleave to aldehydes or ketones [reaction (7-38)], and these undergo further photochemical chain scission as outlined next in Section 7.3.4.3. hn

ROOH ƒƒƒƒ! R0 …CO†R00 , R000 …CO†CH3

…7-38†

The same radical processes may be triggered by impurities in the polymers that form peroxides on irradiation in the presence of oxygen. For example, iron(III) and titanium(IV) present in a polymer initiate peroxide formation

216

7.3 POLYMERS

from molecular oxygen. Exposure to the ozone, formed as a result of air pollution (Section 5.3), also leads to peroxide formation. Antioxidants, which react with free radicals, are added to many polymers to slow their rate of degradation. 7.3.4.3 Photodecomposition Triggered by Carbonyl Groups

Carbonyl groups that are present in polymers as a result of the decomposition of peroxides or are incorporated into the polymer during synthesis absorb UV light at 300±325 nm and initiate reactions leading to the cleavage of the polymer backbone. Two processes can occur, called Norrish type I and Norrish type II. In the type I reaction, bond breaking proceeds by a radical pathway (7-39), while a concerted electron shift occurs in the type II reaction (7-40): O R

C

O hn

R′

R +

C

O R′

CO + R′ O H R

C H2C

CHR CH2

hn

and

R

C

C H2C

R′

OH CHR

CH2

…7-39†

R + CO

O H R

+

R

+

C CH2

CHR

…7-40†

CH2

Many polymers contain small amounts of carbonyl groups that are formed by the decomposition of peroxides, which initiate the slow decomposition of the polymer. For example, unstabilized 2.5-mil-thick ®lms of polyethylene fragment in less than 90 days in the summer Texas sun. It should be noted that this polyethylene is only ``fragmented,'' not totally broken down. Polymers have been prepared in which carbonyl groups were purposely incorporated into the chain to facilitate their extensive photochemical degradation. Polystyrene cups in which 1% of the styrene units also contained a ketone grouping broke down to a wettable powder after standing outside in the sun for 3 weeks. Currently a copolymer of ethylene and carbon monoxide is being used to make the plastic strap that holds beverage cans in a six-pack because it undergoes photochemical decomposition in sunlight. This addresses the problem of wildlife getting caught in this strap as well as its general lack of environmental aesthetics. 7.3.4.4 Hydrolysis

Polyesters, polyamides, and polyurethanes undergo slow hydrolytic degradation to form the corresponding acid and amine or alcohol. This random process does not usually result in the loss of the strength of the polymer.

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

217

However, the rate of cleavage increases with time because the carboxyl and amine or alcohol groups that are formed serve as catalysts to cleave the ester or amide groupings tethered in their vicinity. These catalyze chain scission and loss in the strength of the polymer. The extent of chemical cleavage is also dependent on the physical properties of the polymer. Polymers with a high degree of crystallinity are less susceptible to cleavage than amorphous ones. The crystalline phase is less accessible to penetration by water, so there is less chance that hydrolysis will occur. Biodegradation, to be discussed next, often involves an enzymatic acceleration of the hydrolytic process.

7.3.5 Biodegradation Since biodegradation requires metabolism by microorganisms present in the environment, most of the biodegradable polymers contain functional groups that are subject to attack by microbial enzymes. This means that these polymers contain ester or amide groups that can be hydrolyzed or linear chains that can be oxidatively cleaved by the process described for linear surfactants (Section 7.2.4). A major problem is the inability of microorganisms to ingest high polymers through their cell walls; it is generally not possible for a microorganism to ingest a molecule that has a molecular weight greater than about 500 Da. Some microorganisms that degrade polyesters secrete esterases, enzymes that catalyze the hydrolysis of ester groups, which break the polymer into smaller fragments that can then be ingested. As noted earlier, polyesters also undergo slow hydrolysis at the ester bond in the environment, which will provide smaller, ingestible fragments. Other processes of chemical degradation may also provide fragments small enough to be biodegraded. Synthetic polymers in commercial use that undergo biodegradation in the presence of molecular oxygen were listed in Figure 7-4. These constituted about 2% of the total U.S. plastics production in 1992 and are mainly polyesters. Poly(ethylene glycols) are prepared from ethylene oxide by a process similar to that outlined for nonylphenol ethoxylates (Section 7.2.3.3). Poly (ethylene terephthalate) (Figure 7-3), is a polyester manufactured in large amounts that does not undergo biodegradation, apparently because its aromatic rings do not bind in the catalytic sites of the microbial esterases. Poly(b-hydroxybutyrate) (PHB) and the copolymer of b-hydroxybutyrate and b-hydroxyvalerate (PHBV) (Figure 7-4) are unique in that they are synthesized by microorganisms. These polymers are prepared and stored in the cell in granules. When grown under conditions where nitrogen is a limiting nutrient, the microorganisms produce 30±80% of their cell weight as granules that contain mainly PHB. The genes for the enzymes required to produce PHB have been cloned and expressed in E. coli and in a plant.

218

7.4 CONCLUSIONS

PHB is a brittle polymer that may be used in plastic soft drink bottles but is dif®cult to mold because its melting point and decomposition point are almost the same. It has been possible to induce the microorganisms to prepare the copolymer PHVB by adding some b-hydroxyvalerate to their growth medium. The PHVB formed is more malleable than PHB and has physical properties similar to those of polypropylene. Now manufactured in Great Britain, it is used for making products that are marketed on the basis of their ``environmentally friendly'' or ``green'' image (e.g., shampoos, razors, writing pens). In 1999 it was reported that a genetically engineered plant (oilseed rape) produced PHVB directly. This process is not economically feasible at present, but it does suggest the possibility of the future preparation of polymers using renewable resources. A polyethylene containing 5±20% starch granules is used in the manufacture of shopping bags that are claimed to be biodegradable. The starch granules are degraded by fungi and bacteria. Biochemical degradation of the starch granules from the plastic ®lm enhances its permeability to other reactants. Other additives such as transition metals may also be added to the polyethylene to enhance the photodegradation of the polyethylene via hydroperoxides (Section 7.3.4.2). It is not clear whether all the polyethylene is eventually completely degraded to biomolecules like acetate (Section 7.2.4).

7.4 CONCLUSIONS The environmental problems associated with nonbiodegradable surfactants have been solved with the design of biodegradable replacements. A potential problem with biodegradable surfactants is the eutrophication of lakes due to the buildup of organics resulting from the microbial degradation process. Since, however, the principal cause of most lake eutrophication is runoff of organic waste (manure) and fertilizer from farms, the role of surfactants in this problem appeare to be minor. Polymers derived from petroleum will continue to predominate into the twenty-®rst century. It is likely that new technology will be developed to recycle a greater proportion of the materials. The extent of the recycling may depend on whether ``cradle to grave'' responsibility is mandated for the company that initially synthesizes the polymer. Not all synthetic polymers will be used in a way that permits ef®cient recycling. Research in progress suggests that it may be possible to devise biodegradable polymers for these uses as long as they can be subjected to decomposition in an aerobic environment such as that present in composting. Although progress has been made in the synthesis of biodegradable polymers, these materials cost more and, in general, their properties are not as useful as those prepared from petroleum feedstocks.

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

219

This is a rapidly developing area, so it appears likely that biodegradable polymers will assume an increasingly larger percentage of the polymer market.

Additional Reading Soaps, Detergents, and Synthetic Surfactants Ainsworth, Susan J. Soaps and detergents, Chem. Eng. News, p. 34, Jan. 24, 1994. (A summary of industrial trends in the soap and detergents is published annually in the January issue of Chemical & Engineering News.) Davidsohn, A. S., and B. Milwidsky, Synthetic Detergents, 7th ed. Longman Scienti®c and Technical, New York, 1987. Degradation of Synthetic Organic Molecules in the Biosphere. National Academy of Sciences, Washington, DC, 1972. Meloan, C. E., Detergents, soaps, and syndets, Chemistry 49(7), 6 (1976). Swisher, R. D., Surfactant Biodegradation, 2nd ed., revised and expanded. Dekker, New York, 1987.

Polymers Aguado, J., and D. Serrano, Feedstock Recycling of Plastic Wastes. Royal Society of Chemistry, Cambridge, U.K. 1999 192 pp. Alexander, Martin, Biodegradation and Bioremediation. Academic Press, San Diego, 1994, pp. 278±280. Ching, Chauncey, David L. Kaplan, and Edwin L. Thomas, eds., Biodegradable Polymers and Packaging, Technomic, Lancaster, PA, 1993. Dawes, Edwin A., ed., Novel Biodegradable Microbial Polymers. Kluwer Academic, Dordrecht, 1990. Hamid, Halim, S. Mohamed B. Amin, and Ali G, Maadhah, eds., Handbook of Polymer Degradation. Dekker, New York, 1992. Satyanarayana, D., and P. R. Chatterji, Biodegradable polymers: Challenges and strategies, J. Macromol. Sci. Rev. Macromol. Chem. Phys.,
, 349±368 (1993). Vert, M., J. Feijen, A. Albertsson, G. Scott, and E. Chiellini, eds., Biodegradable Polymers and Plastics. Royal Society of Chemistry, Cambridge, U.K., 1992.

EXERCISES 7.1. (a) What structural units are cleaved from a soap when it decays in a sewage disposal plant or in the environment? Illustrate by equations the cleavage of one unit from the salt of octadecanoic acid [CH3 …CH2 †16 COOH]. (b) Identify the agent(s) in a sewage plant or environment responsible for this degradation.

,

EXERCISES

(c) Why were some surfactants slow to break down in a sewage plant and in the environment? 7.2. (a) Surfactants and some hydrocarbons are metabolized by certain microorganisms in the environment. Write one or more reaction(s) to illustrated the overall process by which one fragment is cleaved by these microorganisms from hydrocarbon with the formula CH3 …CH2 †8 CH3 and from surfactant of general formula CH3 …CH2 †16 CH2 OSO23 (b) Explain with words and=or equations why the following compound is resistant to microbial degradation. Be speci®c in your answer. CH3CHCH2CHCH2CHCH3 CH3

CH3

CH3

7.3. Outline the steps in the free-radical polymerization of styrene. 7.4. (a) Which of each of the following pairs of compounds degrades more rapidly in the environment? CH3 …CH2 †8 CH3 and CH3 …CH2 †48 CH3 , polyethylene and polyhydroxybutyrate, branched-chain nonylbenzenesulfonate and linear nonylbenzenesulfonate, n-decane and a linear hydrocarbon of formula C50 H102 . (b) Give one reason for your answer based on the structure of the compound. (c) Use chemical equations to illustrate the ®rst step by which each of the more environmentally reactive compounds degrades in the environment. 7.5. Chemists have devised synthetic polymers with a wide array of uses. Some are stronger than steel and many are much less expensive than paper. (a) What problems are associated with the disposal of these polymers on land and in the ocean? (b) Many polymers, even the so-called degradable ones, don't breakdown in these environments. Why not? (c) What problems are associated with recycling synthetic polymers? 7.6. Materials constructed of the following polymers were thrown away in a forest by slovenly campers. (a) Which of them will have been degraded by environmental in a year's time? Explain your answers. (b) Give the reaction pathway by which degradation occurred for those that did break down (n ˆ 1000 in every example).

221

7. SOAPS, SYNTHETIC SURFACTANTS, AND POLYMERS

O

O Polylactate

OCHC

Polyalanine

n

HNCHC CH3

CH3 Polyacrylonitrile

n

CH 2CH

n

Polydichlorostyrene

CHCH2

n

CN Cl Cl

(c) Write the reaction pathway for the polymers that decay at a signi®cant rate in the environment. 7.7. Of the garbage that is dumped in the ocean by ships mainly the plastic ware (bottles, spoons, cups, etc.) ends up on beaches. Why aren't the other items present in garbage (paper, food, etc.) also washed up on the beaches?

8 HALOORGANICS AND PESTICIDES

8.1 INTRODUCTION Haloorganic compounds have many uses, such as pharmaceutical agents, ®bers, building materials, agricultural chemicals, solvents, and cleaning agents. Many of these compounds are inexpensive to manufacture and are used in large quantities. Many were manufactured and deliberately distributed in the environment as pesticides to control plant and insect pests. Some were allowed to be released in the environment because their long-term toxicity and environmental hazards were not understood. Yet others reached the environment because they are volatile or because they were discarded in open dumps and land®lls. The scope of the environmental problems associated with the extensive use of slowly degrading haloorganics has been known for many years, and steps have been taken to remedy some of these problems. The environmental stability of some of these compounds is high, and the manufacture of the more stable compounds has been banned in the United States and some other countries. The toxicity and environmental problems associated with some of these compounds are appreciable. Examples include chloro¯uorocarbons, polychlorinated biphenyls (PCBs), and organochlorine pesticides. 223

224

8.2 ENVIRONMENTAL DEGRADATION

We begin the chapter with a discussion of the reactivity of haloorganics under environmental conditions. The chemistry and environmental problems due to several types of haloorganic, which are now or have been an environmental problem, are considered. It is not possible to discuss every type of commercial haloorganic, but the goal is to provide suf®cient breadth of coverage to permit the reader (1) to estimate the relative reactivity of these and other haloorganics under environmental conditions, (2) to understand the scope of their effect on the environment, and (3) to understand how these environmental problems are currently being addressed. Because many chloroorganics are pesticides, the chapter includes a discussion of general pesticides and other methods of pest control. 8.2 ENVIRONMENTAL DEGRADATION There are many environmental processes that may cause the degradation of haloorganic and other organic compounds. These processes may result in their being converted to nontoxic substances or in some instances more toxic compounds. These processes include the following.
Hydrolysis with water. Water reacts with the functional groups attached to a hydrocarbon backbone such as chloro groups, esters, and other derivatives of carboxylic and phosphoric acids. Often the hydrolysis of these functional groups makes the organic part of the molecule more soluble in water, hence more amenable to degradation by microorganisms. Water hydrolysis is one of the more important environmental reactions because most organics eventually end up in solution or in the sediments of rivers, lakes, and=or oceans.
Reaction on mineral surfaces. Many organics bind to the surfaces of minerals in sediments or to the organic material that is bound to a mineral surface (Section 12.1). Some of these minerals catalyze the decomposition of substituted organics. For example, sedimentary clay minerals catalyze the hydrolysis of some chloroorganics. Others bind the organic compounds preventing them from migrating in the environment.
Photolysis. The photochemical reaction of organics occurs mainly with volatile organic compounds, but it is occasionally important for solids as well, especially if they are used in agriculture. These pesticides and herbicides are sprayed on the surfaces of plants, where some may be degraded by solar radiation. In addition to degradation by direct photolysis, volatile organics may be decomposed by the radicals produced by the photolysis of other atmospheric gases.
Oxidation by molecular oxygen. Unsaturated compounds are usually the most susceptible to oxidation by molecular oxygen. Sometimes the oxygen is

225

8. HALOORGANICS AND PESTICIDES

activated by UV light to the singlet excited state, in which it is more reactive than triplet ground state oxygen (Section 5.2.2).
Microbial degradation. The metabolic machinery of microorganisms is the most powerful environmental force for the degradation of organics. Microorganisms are sometimes able to break down compounds, that are not normally present in the environment into compounds that are part of the natural biosphere. Such a transformation results in the conversion of a pollutant to a nonpollutant: the solution of an environmental problem. Compounds that are readily degraded by microorganisms are not generally an environmental concern unless their degradation results in abnormally high levels of organic material. It is rare for the environmental processes described in the ®rst four items just listed to result in the conversion of a nonbiodegradable compound to one that is part of the natural biosphere. Rather, these nonbiological processes convert a nonbiodegradable compound to one that is susceptible to degradation by microorganisms (®fth process).

8.3 CHEMISTRY OF CHLORINATED ORGANIC COMPOUNDS 8.3.1 Synthesis Organochlorine derivatives are prepared industrially by the direct chlorination of hydrocarbons. RH + Cl 2

RCl + HCl

8-1

The mechanism of this reaction is discussed in many elementary chemistry texts, so it is only brie¯y outlined here. It is a free-radical process initiated by atomic chlorine generated by light or heat (reaction 8-2). hu or ∆

2Cl

8-2

RH + Cl

R + HCl

8-3

R + Cl2

RCl + Cl

8-4

RCl

8-5

Cl 2

R + Cl

Chlorination is also useful in the preparation of organochlorine compounds such as 1,3-dichloro-1-propene, which are effective in killing nematodes (soil worms). The overall reaction is CH2

CHCH3 + 2Cl2

ClCH

CHCH2Cl + 2HCl

8-6

226

8.3 CHEMISTRY OF CHLORINATED ORGANIC COMPOUNDS

The reaction proceeds via the stable allylic free radical formed by hydrogen abstraction with a chlorine atom (8-7). This radical reacts further with Cl2 to give allyl chloride (8-8), that in turn adds Cl2 to yield 1,2,3-trichloropropane (8-9). CH2

CH2

CHCH3 + Cl

CH2 CHCH2 + HCl

CHCH2 + Cl2

CH2

CH2

CHCH2Cl + Cl2

CHCH2Cl + Cl

ClCH2CHCH2Cl Cl

8-7 8-8 8-9

Elimination of HCl from 1,2,3-trichloropropane yields 1,3-dichloropropene. An 87% yield of approximately equal amounts of the cis and trans isomers of 1,3-dichoropropene is obtained in this reaction, along with a 12% yield of 3,3-dichloropropene (8-10). CH2

CHCH2Cl + Cl2

CH2

CHCHCl2 + HCl

8-10

The degree and position of halogenation of hydrocarbons depends on the ease of hydrogen abstraction (or stability of the corresponding radical) at each carbon atom and the reaction conditions, such as the ratio of chlorine to hydrocarbon. More vigorous conditions are required to chlorinate aromatic compounds than aliphatic compounds. The aromatic chlorination reaction proceeds by an ionic pathway. For example, polychlorinated biphenyls are prepared from biphenyl by direct chlorination using ferric chloride as a catalyst (8-11). The mechanism involves the initial formation of a chloronium ion [reaction (8-12) ] that undergoes an electrophilic addition to the aromatic ring system as illustrated in reaction (8-13) with benzene. Cl + Cl2 (excess)

FeCl3

Cl

Cl

Cl + HCl

8-11

Cl (One of many products)

Cl2 + FeCl3 Cl Cl

H

FeCl4− + Cl+

8-12 Cl H

8-13

Chlorination of some organics takes place under conditions used to disinfect water with chlorine gas. The chlorine is converted to hypochlorous acid

227

8. HALOORGANICS AND PESTICIDES

(HOCl), which is the oxidizing and chlorinating reagent discussed later [Section 11.5.1] reaction (11-11) ]. Compounds with aliphatic double bonds or aromatic compounds containing phenolic hydroxyl groups are chlorinated under these conditions. But aromatic compounds such as biphenyl are not chlorinated.1 8.3.2 Reactions The aliphatic organochlorine compounds are generally more reactive than the corresponding aromatic derivatives. Two limiting reaction pathways (displacement and elimination) are observed for aliphatic chloro derivatives in the presence of nucleophilic reagents. 8.3.2.1 Displacement Reactions

Displacement may proceed by unimolecular (SN 1) [reactions (8-14) and (8-15) ] or bimolecular (SN 2) [reaction (8-16) ] reaction pathways. The ratelimiting step of the SN 1 reaction is ionization of the alkyl halide to the planar carbocation (8-14), while the rate of the SN 2 reaction is proportional to the concentrations of both alkyl halide and nucleophile (8-16). CH3

CH3

CH3

C CH3

Cl

CH3

OH

fast

C

8-14

CH3

8-15

OH

CH3

H C

CH3 CH3

CH3

CH3

Cl

CH3

CH3 C

CH3 C

OH

HO

H C

Cl

Cl

CH3CH2

CH2CH3 Transition state CH3

H

Cl

C HO 1

8-16

CH2CH3

R. A. Larson and Eric J. Weber, Reaction Mechanisms in Environmental Organic Chemistry, Chapter 5, pp. 275±358. CRC Press, Boca Raton, FL, 1994.

228

8.3 CHEMISTRY OF CHLORINATED ORGANIC COMPOUNDS

The mechanism of the displacement reaction is determined by the solvent, the displacing agent, and the structure of the chloroorganic molecule. The SN 1 (carbocation) mechanism is favored by polar solvents that stabilize the ionic intermediates or when the displacing agent is a poor nucleophile such as water. Carbon compounds with sterically hindered halogens resistant to direct (SN 2) displacement or containing tertiary, allylic, and benzylic halogens (which ionize to stabilized carbocations) usually react by an SN 1 pathway. The ease of ionization of a carbon-halogen bond increases in the order F < Cl < Br < I. This trend re¯ects the decreasing strength of the carbonhalogen bond (Table 8-1). The CÐF bond is so strong that ionization is never observed under environmental conditions; hence carbon±¯uorine bonds present in ¯uorocarbons are not cleaved in the environment. 8.3.2.2 Elimination Reactions

Two limiting reaction mechanisms are available for the elimination reaction: a unimolecular (E1) pathway [reactions (8-14) and (8-17) ] and a bimolecular (E2) pathway [reaction (8-18) ]. The extent of ole®n or alcohol formation is determined by steric effects at the carbocation and the stability of the ole®nic product. CH3 CH3

Base + CH3CH2CH2Cl

CH3

C–CH3

C

H

8-17

CH3

Cl CH

CH3 CH2

CH3 C

CH2

H

CH2 + H Base + Cl

H

8-18

Base Transition state

The factors that favor the SN 1 reaction also favor E1 elimination because the same carbocation intermediate is involved (8-14). The relative proportion of elimination to displacement is determined by the relative nucleophilicity and basicity of the group attacking the carbocation. 8.3.2.3 Predominant Chemical Reaction Pathways in the Environment

When haloorganics are in the environment, and not absorbed by a microorganism, plant, or animal they are usually in the presence of water, that has a moderate pH 7  2 and very low concentrations of other reactants. Consequently SN 2 or E2 reactions will not be observed because the concentration of nucleophiles, acids, and bases is very low. Ionization reactions are favored

229

8. HALOORGANICS AND PESTICIDES

TABLE 8-1 Bond Dissociation Energies and Electronegativities of CH3 X Bond dissociation energies Compound CH3 H CH3 F CH3 Cl CH3 Br CH3 I

kcal=mol 104 108 84 70 56

kJ=mol

Atomic electronegativity of X

425 452 352 293 234

2.1 4.0 3.0 2.8 2.5

Source: Adapted from R. T. Morrison and P. N. Boyd, Organic Chemistry, 6th ed. Prentice Hall, Englewood Cliffs, NJ, 1992.

in water because its solvation of ions and high dielectric constant stabilizes the ionic intermediates. Thus SN 1 and E1 reactions are usually observed. The E2 elimination is observed with strong bases in nonpolar solvents and is not likely to take place under environmental conditions. For example, the dehydrochlorination of DDT and DDT analogues with sodium hydroxide proceeds by an E2 mechanism in 92.6% ethanol [see reaction (8-19) ]. The second-order rate constant decreases by 50% in going from 92.6% ethanol to 76% ethanol. The higher polarity of 76% ethanol±water favors the carbocation (E1) reaction pathway. The elimination proceeds mainly by an E1 mechanism at neutral pH in aqueous solution: Cl CCl 2

CCl2 Cl

C

Cl

Cl

C

Cl + H 2O + Cl

8-19

H HO

DDE

DDT

Nucleophilic displacement of aryl and vinyl halides is a very slow process that does not occur readily under environmental conditions. The SN 1 or E1 reactions are not observed because the sp2 hybrid carbon atom of the aryl or vinyl halide is more electronegative than the sp3 hybrid and cannot stabilize a positive charge and become a carbocation. Furthermore, the lone pairs of electrons on the chlorine participate in the bonding and strengthen the bond as shown in the following resonance structures.

230

8.3 CHEMISTRY OF CHLORINATED ORGANIC COMPOUNDS

Cl

Cl

Cl

Cl

Thus the ground states of the vinyl and aryl halides are more stable than the corresponding ground states of aliphatic halides. This results in a greater energy of activation EA  for carbocation formation and a slower rate of reaction. This is shown qualitatively in Figure 8-1. The reactivity of aryl halides is enhanced by electron-withdrawing groups. For example, a nitro substituent greatly accelerates the rate of displacement of aryl-bound halogens: Cl NO2 OH NO2 HO

Cl NO2

HO

Cl

NO2

HO

Cl

NO2

8-20 NO2

NO2

NO2

OH NO2 Cl NO2

This is due to the formation of an intermediate that is stabilized by the electron-withdrawing substituents. Halide ion displacement from an aromatic ring containing electron-withdrawing groups might thus occur under environmental conditions.

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8. HALOORGANICS AND PESTICIDES

Carbocation intermediate

Free energy

EA1 Alkyl halide

EA2

Vinyl or aryl halide Products

Reaction coordinate

FIGURE 8-1 Reaction coordinate for the conversion of halogenated organics to products by SN 1 or E1 processes.

8.4 MICROBIAL DEGRADATION OF ORGANICS Biodegradation is the key to the destruction of organic compounds in the environment (Section 8.2). Proteins and nucleic acids of dead plants and animals are degraded rapidly because they are metabolized by microorganisms prevalent in the environment. XenobioticsÐcompounds that occur rarely in the environment, such as crude oil, nylon or polychlorinated biphenylsÐeither are not degraded or are degraded slowly because the population of microorganisms available to metabolize them is small. The presence of xenobiotics in the environment may promote the growth of strains of microorganisms that do metabolize these compounds. Microorganisms mutate rapidly, so in some cases there is a mutant that can live by metabolizing the xenobiotic. This is why microbiologists who are looking for a population of microorganisms that degrade a particular xenobiotic search the soil samples in the vicinity of a spill of that compound. The degradation of xenobiotics is usually carried out by a cooperating group of microorganisms called a consortium. Different steps in the degradation are carried out by different microorganisms. For example, the degradation of 3-chlorobenzoate is performed by three different groups of bacteria, as follows:

232

8.4 MICROBIAL DEGRADATION OF ORGANICS

COO

Cl

COO H2 Step 1

Step 2

CH3COO

H2

CH4 Step 3

CO2

8-21

CO2 Cl

The hydrogen generated in step 2 is utilized by the group of microorganisms doing the reductive dehalogenation in step 1 in the process outlined in reaction (8-21). The degradation of organic materials to inorganic compounds of C, H, N, P, the process of mineralization, is the ultimate goal of the degradation of xenobiotics. Mineralization is usually measured by the conversion of carbon to CO2 . But biodegradation may result in the intermediate conversion of the carbon to new microorganisms, not achieving mineralization until these intermediate products die. This is not a concern, since the realistic goal of biodegradation is the conversion of a xenobiotic compound to a biotic one that is readily metabolized by a large population of microorganisms, hence will not accumulate in the environment. These biological compounds will eventually be degraded to CO2 . For example, the acetate formed in the degradation of 3-chlorobenzoate is readily metabolized by both anaerobic and aerobic microorganisms. The crucial step in the degradation of 3-chlorobenzoate is the reductive elimination of chloride ion, a reaction that is carried out by relatively few microorganisms. Both anaerobes and aerobes degrade xenobiotics. Anaerobes often use reductive processes to degrade organics, and aerobes use oxidative processes. Both carry out other processes in which there is no change in the oxidation state of the xenobiotic.

8.4.1 Reductive Degradation The anaerobic dehalogenation of a pesticide was discovered during an investigation of the loss of potency of g-hexachlorocyclohexane [Lindane: see Section 8.9, reaction (8-40) ] in a cattle tick bath. The cattle were made to swim through the bath containing hexachlorocyclohexane to kill the ticks. Since the chemical is expensive, the same bath was used for several years. The potency of the bath decreased slowly with time, but when fresh pesticide was added to it, the rate of loss of the hexachlorocyclohexane dropped more rapidly. The rapid loss in activity was traced to microorganisms, which evolved in the bath over several years. These microorganisms metabolized the hexachlorocyclohexane by removal of its chlorines as chloride.

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8. HALOORGANICS AND PESTICIDES

Bacterially mediated reductive dehalogenation is an important pathway for the destruction of unreactive haloorganics. The reaction usually proceeds in anaerobic environments such as marine sediments and land®lls with the replacement of halogens with hydrogens. The principal pathway for the reductive dechlorination of 2,3-dichlorobenzoate is shown in reaction (8-22). The benzoate formed is readily degraded by other microorganisms, as shown in Section 6.4. COO

COO

COO

Cl

8-22

Cl Cl

Cl Cl

Reductive dechlorination is an important ®rst step in the degradation of heavily chlorinated organics like pentachlorophenol (PCP). PCP is rapidly converted to tetrachlorophenols, but the subsequent loss of chloride in the process of forming tri-, di-, and monochlorophenols proceeds much more slowly than the initial loss of chloride ion. The faster initial rate re¯ects the higher oxidation potential of PCP, which makes it easier to reduce than its more lightly chlorinated metabolites. The reductive dehalogenation of aliphatic compounds has also been observed. For example, 1,1,1-trichloroethane (methylchloroform) can be reduced to the corresponding dichloro derivative: (Cl)3CCH3

H

2e

(Cl)2CHCH3

Cl

8-23

8.4.2 Oxidative Degradation The energy derived from the oxidation of xenobiotics with atmospheric oxygen drives the process of oxidative degradation. These oxidations occur mainly with lightly chlorinated chloroorganics because they require the attack of an electrophilic oxygen on an electron-rich center such as an aromatic ring or a double bond. The delocalization of these electrons by electronegative chlorine atoms decreases the electron density on the aromatic ring; hence these compounds are less readily oxidized by molecular oxygen. The overall oxidative degradation of chlorobenzene is shown in reaction (8-24).

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8.5 TOXICITY

COOH COOH H

OH OH

OH

H b

a Cl

OH

Cl

c d

Cl OH

8-24

Cl COOH COOH Cl

In step a, a microbial dioxygenase enzyme catalyzes the formation of a cisdihydrodiol, which is then oxidized (step b) to a halogenated catechol. Enzyme-catalyzed oxidative ring cleavage takes place either between the two phenol groups (step c) or adjacent to one of the phenol groups (step d) to give dicarboxylic acids, which are readily degraded to simpler compounds and eventually to CO2 , H2 O, and Cl . 8.4.3 Hydrolytic Degradation Hydrolytic cleavage of halogens, esters, amides, and other groupings are catalyzed by both aerobes and anaerobes. Dichloromethane (methylene chloride), a compound that decomposes very slowly in the presence of water, is hydrolyzed by microorganisms to formaldehyde. The enzyme-catalyzed reaction usually proceeds by the SN 2 displacement of chloride ion by the thiol peptide glutathione (G-SH). The resulting intermediate is hydrolyzed to glutathione and formaldehyde: H2 O

G-SH  CH2 Cl2 ƒƒG-SCH2 Clƒƒ G-S  CH2 ƒƒ G-SH  CH2 O  H   8-25  HCl Cl

The microorganisms that catalyze this reaction utilize formaldehyde as an energy source. 8.5 TOXICITY Acute or immediate toxicity to humans and animals is not usually a problem for most commercial haloorganic compounds. The toxicity associated with

8. HALOORGANICS AND PESTICIDES

235

some haloorganics is of the chronic type, where the deleterious effect appears 2±30 years after the initial exposure. For example, vinyl chloride, the monomer polymerized to poly(vinyl chloride) (Figure 7-3), evidently caused cancer in factory workers making the polymer twenty years after they started working with it. Since these workers all contracted an unusual type of liver tumor that was not observed in the general population, it was concluded that vinyl chloride was the causative agent. Most commercial halocarbons are nonpolar compounds that are removed from the bloodstream by the liver. There, their presence induces the synthesis of the enzyme cytochrome P-450, which catalyzes the oxidative degradation of the nonpolar organics in the liver. However, if the compounds are heavily chlorinated, they may have high oxidation potentials and are oxidized slowly, or not at all, by cytochrome P-450 (Section 7.2.4). The high levels of this enzyme that are induced in the liver catalyze the oxidation of other nonpolar organics such as steroids. Since other steroid hormones are produced by cytochrome P-450 oxidation, the presence of excess cytochrome P-450 can change the normal hormonal balance. Some of these haloorganics have many deleterious health effects other than causing cancer. Low levels can cause endocrine, immune, and neurological effects. Haloorganics vary dramatically in chronic and acute toxicity according to structure, and examples of speci®c problems are presented when selected types of compound are discussed in the sections that follow.

8.5.1 Environmental Hormones The possible role of industrial chemicals in human health was debated extensively in the 1990s. Some chronic effects on humans have been anticipated since the observation of the decline in the number of eagles and hawks in the 1960s and 1970s, that correlated with the buildup of chloroorganics in the environment. There was some reassurance that humans might not be affected by these compounds because of the resurgence of the birds in the 1980s following the ban of the use of DDT in 1972. However, there were still reports of the decrease in populations of some birds and the apparent feminization of males in which enhanced levels of chlorinated organics were found. The observation of abnormal sexual development of a number of forms of wildlife and the detection of higher levels of chloroorganics in the same animals led to the proposal that some industrial chemicals have hormonal activity that mimics or inhibits the activities of the sex hormones. Estrogen, a mixture of three steroid hormones, has essential roles in both males and females. A speci®c ratio of estrogen to androgen (male hormones) is required during prenatal and postnatal development for sex differentiation and for the development of reproductive organs. In females estrogen also prepares the

236

8.5 TOXICITY

uterus to accept the fertilized egg, helps with lactation, and lowers the risk of heart attacks, but stimulates the development of uterine and breast cancer. The presence of too much estrogen in males inhibits sperm production and the development of the testes. In a number of instances industrial chemicals or their breakdown products have been shown to have estrogen-like activity that interferes with the sex hormones in wildlife. For example, the feminization of seagulls was attributed to the higher levels of chloroorganics in these birds. PCBs appear to exert the same effect in terns living near a toxic waste site containing these chemicals. PCBs also demonstrate estrogen-like activity in turtles. Laboratory studies have established that o,p-DDT, p, p -methoxychlor [structure given in reaction (8-35) ], kepone, and some PCBs and the phenols derived from them are O

Cl

Cl Cl Cl Cl

Cl Cl Cl

Cl Cl Kepone

estrogen mimics. Nonchlorinated organics have also been shown to be estrogen mimics. Examples include bisphenol A, a degradation product of polycarCH3 HO

C

OH

CH3 Bisphenol A

bonate polymers, and alkylated phenols such as p-nonylphenol, a degradation product of polyethoxylate detergents (Section 7.2.2.3). The interpretation of the effect of a mixture of environmental compounds found in humans on their health is complicated by the varied biological responses triggered by the presence of the compounds. Some industrial compounds have been shown to have antiestrogenic effects. These include 2,3,7,8tetrachlorodibenzo-p-dioxin [TCDD: see Section 8.10.3, reaction (8-58) ] and polychlorinated benzofurans [Section 8.7.3, reaction (8-30) ]. In principle, these compounds could negate the effects of the environmental estrogens. Another problem with TCDD is that it may cause endometriosis, a disorder in women in which tissue migrates from the uterus to the abdomen, ovaries, bowels, and bladder. This can result in internal bleeding and infertility. The

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8. HALOORGANICS AND PESTICIDES

possible role of TCDD in endometriosis was suggested by a long-term study of the reproductive effects of TCDD in monkeys. TCDD was included in the diet of 24 female monkeys for four years and then no more was administered. In the 6-to 10-year period after the initial administration of the TCDD, 3 of the monkeys died of endometriosis. Investigation of the remaining monkeys revealed that 75% of those given a high dose of TCDD had moderate to severe cases of endometriosis, while only 42% of those given a weak dose had the ailment. None of the control monkeys had endometriosis. More recently it has been discovered that DDE, a breakdown product of DDT, has antiandrogen activity. Antiandrogens compete with the male sex hormones for binding at androgen receptor sites and thus inhibit the activity of the androgens. The net result of this inhibition is comparable to the presence of compounds with estrogen activity. It appears likely that the feminization of newborn alligators living in a lake containing high levels of DDE should really be called demasculinization resulting from the antiandrogenic effect of the DDE. There is general agreement on the assignments of estrogenic, antiestrogenic, or antiandrogenic properties to the compounds listed in Table 8-2. Disagreements arise when these data are used to explain recent health problems in humans. For example, the increases in breast cancer observed in older women over the past 50 years have been tentatively attributed to long-term exposure to environmental hormones. The assumption is that since estrogen is a cause of breast cancer, environmental hormones will also cause cancer. Correlations have been reported between the PCB levels in tissue and DDE present in serum in women who have breast cancer, but there is no evidence of a direct link between breast cancer and these compounds. It has also been proposed that the 40% decline in sperm counts in men over the past 50 years is due to exposure to estrogen-like and antiandrogen compounds in the environment. In addition,

TABLE 8-2 Proposed Hormonal Activity of Environmental Compounds Estrogen-like PCBs o,p-DDT Methoxychlor Kepone Toxaphene Dieldrin Endosulfan Atrazine Bisphenol A Nonylphenol

Antiestrogens 2,3,7,8-Tetrachlorodioxin Polychlorinated benzofurans Benzo(a)pyrene

Antiandrogen DDE

238

8.6 CHLOROFLUOROCARBONS, HYDROFLUOROCARBONS, AND PERHALOGENATED ORGANICS

it has been proposed that there is a correlation between the increase in testicular cancer and the presence of estrogen-like compounds in the tissue of males. As in the case of breast cancer, there is no unambiguous link between the medical observations and environmental compounds. An important argument against the important role of environmental chemicals as estrogens in humans is the observation that the cruciferous vegetables (brussel sprouts, cauli¯ower, kale, etc.) contain bio¯avonoids that exhibit estrogenic activity.2 It is calculated that the estrogenic potential of the compounds in these vegetables is 107 times higher than that of the environmental chemicals because they constitute such a high proportion of our diet. Scientists on both sides of the debate agree that more data are required before conclusive statements can be made concerning the importance of environmental estrogens on humans. Many of the persistent organic pollutants (POPs) that are believed to be environmental hormones are still being produced and used in the world. These compounds are carried from where they are manufactured or used around the globe by weather patterns. The United Nations sponsored and adopted a treaty in 2000 intended to end the production of these and other persistent chlorinated compounds throughout the world and to destroy their stocks. This is the ®rst attempt to control these compounds globally. The ``dirty dozen'' compounds include the insecticides aldrin, chlordane, DDT, dieldrin, endrin, heptachlor, hexachlorobenzene, mirex, and toxaphene plus the industrially used polychlorinated biphenyls and the industrial by-products, dioxins and benzofurans. The treaty took effect upon rati®cation by 122 nations in December, 2000. The use of DDT for the control of malaria is the one exception to the ban, since the insecticide is still used for this purpose in Africa, Asia, and South America. The structures and discussions of most of these compounds are given in subsequent sections of this chapter.

8.6 CHLOROFLUOROCARBONS, HYDROFLUOROCARBONS, AND PERHALOGENATED ORGANICS Chloro¯uorocarbons (CFCs) and perhalogenated organics were used for a long time as aerosol propellants, refrigerants, solvents, and foaming agents, but this use has been curtailed. So-called halons, which contain bromine as well as ¯uorines, are still used to extinguish ®res in critical situations such as on aircraft. Most of these compounds are nontoxic, stable, colorless, and non¯ammable: ideal substances for use in a variety of industrial applications. The high stability of these compounds, which made them so attractive to industry, also explains 2

S. E. Safe, Environmental and dietary estrogens in human health: Is there a problem? Environ. Heath Perspect., 103, 346±351 (1995).

8. HALOORGANICS AND PESTICIDES

239

why they are implicated in two major environmental problems, global warming (Section 3.3.3) and the destruction of the ozone layer (Section 5.2.3.2).

8.6.1 Structural Types The chloro¯uorocarbons that were banned from production in the industrialized nations in 1996 (Section 5.2.3.5) are highly halogenated derivatives that do not contain a CÐH bond (e.g., CCl3 F, C2 F2 Cl4 , and C3 F2 Cl6 . The perchlorinated compound carbon tetrachloride (CCl4 ), which had been used extensively as a degreasing and cleaning solvent, is as deleterious to the environment as the CFCs. Methylchloroform (1,1,1-trichloroethane, CCl3 CH3 ), which was also used for degreasing, although it has one-tenth the ozonedestructive power of CFCs, was nevertheless a major contributor to the destruction of the ozone layer because it was used in large amounts in industry. Bromo¯uorocarbons (halons), such as CBrF3 , used to extinguish ®res in military and commercial aircraft, are believed to act in much the same way that tetraethyllead prevents preignition in internal combustion engines (Section 6.7.4), that is, by combining with free radicals and stopping the oxidative chain reaction central to the combustion process. The production of halons that destroy the ozone layer (Section 5.2.3.2) was banned in 1994 in the industrialized countries but will continue in developing nations. There are still large supplies available that, when put to use to ®ght ®res, will eventually end up in the ozone layer. The level of halons in the atmosphere was still increasing in 1998. It is ironic that the same person, Thomas Midgely Jr., invented both chloro¯uorocarbons and tetraethyllead. These compounds, which were highly acclaimed when discovered in the 1920s, made possible the widespread use of refrigerators and automobiles, staples of the American culture and economy. The manufacture and use of leaded fuels in the United States continued until 1995, while the manufacture of chloro¯uorocarbons was halted in 1996. The phaseout in the use of these compounds started some 10±15 years earlier than the ®nal cutoff dates. 8.6.2 Atmospheric Lifetimes
8.6.2.1 Chloro¯uorocarbons and Perhalogenated Organics

Carbon tetra¯uoride (CF4), the most stable of the perhalogenated organics, is estimated to have a lifetime in the environment that exceeds 50,000 yearsÐ 3

The lifetimes referred to in this section are the reciprocal of the ®rst-order rate constant for their degradation. See A. R. Ravishankara and E. R. Lovejoy, Atmospheric lifetime, its application and determination: CFC-substitutes as a case study, J. Chem. Soc. Faraday Trans., 90(15), 2159± 2169 (1994).

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8.6 CHLOROFLUOROCARBONS, HYDROFLUOROCARBONS, AND PERHALOGENATED ORGANICS

about 10 times longer than the history of human civilization. It is formed as a by-product of the production of aluminum by the electrolysis of aluminum oxide in a melt of cryolite (Na3 AlF6 ) (Section 12.2.5). The CF4 is formed by the reaction of ¯uorine with the carbon electrodes at the high temperatures (10008C) and voltages used in the electrolytic process. About 30,000 tons of CF4 is released globally into the atmosphere each year by this process. The presence of strong CÐF and CÐCl bonds and the absence of CÐH bonds are central to the environmental stability of the CFCs and perhalogenated organics. The trends in the energy of dissociation of the carbon±halogen bond of halomethanes show the CÐF bond to be the strongest (Table 8-1). The large energy of dissociation of the CÐF bond is a consequence of the greater overlap of the bonding orbitals because of the similarity in size of the carbon and ¯uorine atoms. In addition, because of its high electronegativity (4.0), the ¯uorine atom reduces electron density on carbon and deactivates the carbon atom for reaction by SN 1 or E1 processes (Section 8.3.2). Because the CÐCl bond is weaker than the CÐF bond, a CFC will react to form a carbocation by ionization of the chlorine atom as follows: Cl

F C

Cl

Cl

F C

Cl

Cl

8-26

Cl

The postulated carbocation intermediate in reaction (8-26) has a very high energy. Consequently, the chloride atom ionizes from the carbon to form the carbocation only at high temperatures. While CCl4 is more reactive than CF4 , the relatively high strength and electronegativity (3.0) of the CÐCl bond (Table 8-1) explains the environmental stability of CCl4 . CFCs and perhalogenated organic compounds are stable in the earth's atmosphere because they do not contain CÐH groups and therefore are resistant to attack by hydroxyl radicals (Section 5.2.3.5). Since abstraction by a hydroxyl radical ( OH) of a chlorine atom from a CFC to form ClOH is not energetically favored, CFCs only react after diffusion up to the ozone layer, where solar UV radiation initiates the dissociation of the chlorine atom (Section 5.2.3.2). The chlorine atom catalyzes the dissociation of ozone. Since CF4 does not contain chlorine or bromine, it does not cause the destruction of the ozone layer, but its global warming potential is several thousand times greater than that of a comparable amount of carbon dioxide (Section 3.1.2). Methylchloroform, an industrial solvent, is a compound whose production was curtailed as a result of the 1987 Montreal Protocol agreement (Section 5.2.3.5). It is not as inert as the chloro¯urocarbons, with a lifetime of 5.2 years

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8. HALOORGANICS AND PESTICIDES

in the Northern Hemisphere and 4.9 years in the Southern Hemisphere. Its atmospheric concentration leveled off in 1991 and started to decrease in 1995. The rapid decay of methyl chloroform is due to its reaction with atmospheric hydroxyl radicals to form CH2 CCl3 (Section 5.2.3.5). It was possible to calculate from these lifetimes that the concentration of hydroxyl radicals in the atmosphere of the Southern Hemisphere is 1510% higher than in the Northern Hemisphere. The annual production of CFCs decreased by 90% in the 1986±1995 time period. Since the lifetimes of many CFCs in the atmosphere are in the range of 50±150 years, limitations on their production will not result in a decrease in their atmospheric concentrations until about 2001±2010 (Figure 8-2). However the global agreement to halt the production and use of chloro¯uorocarbons made in the Montreal Protocol in 1987, and its subsequent modi®cations, have resulted in halting the increase in buildup of stratospheric chlorine in 1994 at one-third the level that might have formed if no controls had been put in place until 2010. It is predicted that the ozone levels will decrease in 2050 to those observed in the time period when the Antarctic ozone hole was discovered (1980±1984: see Section 5.2.3.3).

Cumulative stratospheric chlorine equivalent, ppb 4 Total Methyl bromide chlorine Halons 3 HCFCs Carbon tetrachloride 2 Methyl chloroform 1

CFCs

Chlorine level at which Antarctic ozone hole appeared

“Natural” methyl bromide “Natural” methyl chloride

0 1979 1984 1989 1994 1999 2004 2009 2014 2019 2024 2029 2034 2039 2044 2049 2054

FIGURE 8-2 Projected trend in levels of chlorine, CFCs, HCFCs, and haloorganics in the atmosphere as a consequence of The Montreal Protocol. Redrawn from, ``Looming ban on production of CFCs, halons spurs switch to substitutes,'' Chem. Eng. News, p. 13, Nov. 15, 1993. Used by permission of E.I. du Pont de Nemours and Company. Also see color insert.

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8.6 CHLOROFLUOROCARBONS, HYDROFLUOROCARBONS, AND PERHALOGENATED ORGANICS

8.6.2.2 Hydrochloro¯uorocarbons and Hydro¯uorocarbons

Hydrochloro¯uorocarbons (HCFCs) and hydro¯uorocarbons (HFCs) have been designed to take the place of CFCs, which were banned from production in industrialized nations on January 1, 1996. Many times, a chemist who has prepared a useful but unstable compound is asked to come up with a compound that has similar properties but does not break down. The assignment in the case of the CFCs, however, was to make a less stable substitute that breaks down more rapidly in the environment. The approach used was to include CÐ H bonds in these substitutes for the CFCs so that they would be susceptible to oxidation by hydroxyl radicals in the atmosphere (Section 5.2.3.5). Two examples of the hundreds of HCFCs and HFCs prepared are CH3 CHF2 (HFC-152a) and CF3 CH2 F (HFC-134a). Both have no ozone destruction potential, but both are greenhouse gases. In fact, CF3 CH2 F has about ®ve times the global warming potential of CH3 CHF2 . The global warming potentials of CFCs, like CFCl3 , are about 30 times greater than that of CH3 CHF2 . The atmospheric lifetimes of CH3 CHF2 and CF3 CH2 F are estimated to be 2 and 14 years, respectively, values that are considerable shorter than the 50-to 100-year lifetimes of the CFCs. In addition, since these compounds contain no bromine or chlorine, they will not destroy the ozone layer. There was a concern that the CF3 radical formed in the atmospheric degradation of CF3 CHF2 , and other CFC substitutes that contain the CF3 group, would catalyze the degradation product of ozone, via the formation of CF3 OO. and CF3 O. by reaction with molecular oxygen and ozone, respectively. Laboratory studies and atmospheric models showed that these oxygenated tri¯uoromethyl radicals would react in the lower stratosphere, where they would have a negligible effect on the level of atmospheric ozone. There is also the concern that the tri¯uoroacetic acid, an important atmospheric degradation product of CFC substitutes containing the CF3 group, would accumulate at toxic levels in ecosystems where water evaporates to form concentrated solutions of organic and inorganic compounds. While it has been demonstrated that tri¯uoroacetic acid is not very toxic to humans, plants, and animals, and is degraded by some anaerobic bacteria, there is still concern that it may accumulate in the ecosystems and be toxic to the life there. These conclusions were reached on the basis of modeling (calculations) and have not been veri®ed by experimental studies. The HCFCs and HFCs are not expected to be permanent replacements for chloro¯uorocarbons. Rather, their use is planned until 2020, when they are expected to be replaced by even more benign substitutes. For example, while compounds that contain the CF3 group (e.g., CF3 CHF2 ), do not destroy the ozone layer, they are degraded to CHF3 , which has a 400-year atmospheric lifetime and 8000 times the global warming potential of carbon dioxide. Policy makers expect that chemists will ®nd readily degradable compounds that neither destroy the ozone layer, cause global warming, nor degrade to sub-

8. HALOORGANICS AND PESTICIDES

243

stances that are toxic to any forms of life on earth. These compounds should have the desirable properties of CFCs so that all humans can continue to enjoy all the bene®ts of modern civilization without an increase in the cost of living. It remains to be seen whether these desirable characteristics can be achieved. 8.6.2.3 Other Compounds

Progress toward the goal of producing a new generation of halons for use as ®re retardants has not been as successful as the search for effective replacements for CFCs. The current plan is to carefully husband the available supplies of CF3 Br and CBrClF2 by reserving their use for situations in which other retardants cannot be used while the search for effective replacements continues. There was hope that CF3 I would be a direct replacement of CF3 Br, but the toxicity of the iodide prevents its use in aircraft and other closed environments. The production of halons in 1995 decreased to almost zero in both industrialized countries and in all developing countries except China, where the production increased 2.5-fold between 1991 and 1995. Another ozone-destroying chemical, methyl bromide (Figure 8-2), is used in large amounts as a soil and grain fumigant. It is an excellent agent for the removal of fungi, bacteria, viruses, insects, and rodents from soil prior to planting crops. Unlike many other pesticides, it does not persist in the soil but is decomposed in a few weeks. Even though its atmospheric lifetime is short, its use in large amounts results in the transport of some of the pesticide to the ozone layer. It was proposed in 1992 that methyl bromide is responsible for 10% of the depletion of the ozone layer. The photochemically generated bromine atoms destroy ozone about 50 times more rapidly than do chlorine atoms (5.2.3.2). California, the largest agricultural user of methyl bromide of any U.S. state, released 8  106 kg in 1988. It was proposed in 1992 that the use of methyl bromide in developed nations be phased out in 2005. There is great concern about this proposed ban in the agricultural community because there is no obvious replacement. In 1992 it was found that methyl chloride, methyl bromide, and more highly halogenated methane derivatives are formed in the environment. These compounds are produced by microorganisms living in salt marshes, coastal lands, decaying vegetation and in beds of kelp (seaweed) growing on the ocean ¯oor. This is the principal source of atmospheric methyl chloride, since the compound is not manufactured in large amounts. Methyl chloride is a source of the stratospheric chlorine that destroys the ozone layer (Section 5.2.3.2). Since these compounds have been in the environment for a long time, it is likely that there are microorganisms that metabolize them for their carbon and energy. Indeed, in a ®eld that was fumigated with methyl bromide, microbiologists found an anaerobic microbe that uses this compound as its sole energy source. Other microorganisms were discovered in the environment, both

244

8.7 POLYCHLORINATED AND POLYBROMINATED BIPHENYLS

aerobes and anaerobes, which metabolize these halomethane derivatives. Aerobes oxidize them to carbon dioxide and halide ions. Anaerobes use them to methylate the sul®de ion formed by the reduction of sulfate to generate the volatile dimethyl sul®de. These metabolic pathways proceed more rapidly than the simple hydrolysis of methyl halides to methanol but more slowly than the rate of formation of these haloorganics. These new developments have resulted in extensive study of the sources and sinks of methyl bromide in the environment. Anthropomorphic sources of methyl bromide include its release during fumigation, biomass burning, and combustion of leaded gasoline in automobile engines (Section 6.6). These sources, together with production in the environment, are estimated to put 150  106 kg of methyl bromide into the atmosphere each year. The use of methyl bromide for fumigation releases 41  106 kg a year, or about 30% of the total amount released into the atmosphere. It is possible, however, to reduce the amount emitted during soil fumigation by a factor of 10 by covering the ®elds with a sheet of nonpermeable polymer while the methyl bromide is injected into the soil. The polymer sheet prevents the escape of methyl bromide to the atmosphere. If the ®eld is covered for several weeks, the methyl bromide decomposes and is not released when the sheets of plastic are removed. If this practice is shown to be applicable on a large scale, it may not be necessary to ban the use of methyl bromide as an agricultural fumigant. At present there are no plans to rescind the ban on the production of methyl bromide in industrialized countries.

8.7 POLYCHLORINATED AND POLYBROMINATED BIPHENYLS Polychlorinated biphenyls (PCBs) were ®rst used industrially in the 1930s, but their use was not widespread until the 1950s. Their extreme stability made them especially effective in many applications. For example, they are resistant to acids, bases, heat, and oxidation. This stability had prompted their use as heat exchange ¯uids and dielectrics in transformers and capacitors. They were also used in large amounts as plasticizers and solvents for plastics and printing inks and in carbon paper. It is estimated that in the 50-year period of their use, over 1.4 billion pounds was manufactured and several hundred million pounds released in the environment. PCBs were ®rst available commercially in the United States in 1929. The last major manufacturer of PCBs was Monsanto, under the trade name of Arochlor. These products are identi®ed by a four-digit number; the ®rst two digits indicate if it is pure or a mixture, and the last the second two digits designate the weight percent chlorine present. The annual sales of Arochlors increased from 40 million pounds in 1957 to 85 million pounds in 1970. The cumulative U.S. production is estimated at one billion (109 ) pounds. World production

8. HALOORGANICS AND PESTICIDES

245

was 200 million pounds in 1970. Because of the increasing environmental concerns, Monsanto stopped selling Arochlors in 1970 for use where they could not be recovered and terminated manufacture of them completely in 1977 when the EPA recommended that PCBs not be used as heat transfer ¯uids in the production of foods, drugs, and cosmetics. PCB production has been banned in most of the industrial nations of the world. Russia, the principal exception, claims that because all its transformers were built on the use of PCBs as the dielectric, it must continue to manufacture PCBs for these transformers until 2005. The government has pledged to destroy all the unused stock of PCBs in 2020. Thus it appears likely that Russia will be a major source of PCBs in the environment in the twenty-®rst century. PCB manufacture also continues in some nonindustrialized countries in the world.

8.7.1 Environmental Problems The stability of PCBs, which makes them so useful commercially, also results in their persistence in the environment. The ®rst report that these compounds were prevalent and were being ingested by aquatic life came in 1966, when Jensen detected PCBs in ®sh. Since the production of PCBs has been banned in the United States, the current sources in the environment are evaporation from land®lls, incineration of household trash in backyard barrels, volatilization from lakes and other repositories, and synthesis and use elsewhere in the world. For example, since PCBs have been dumped into and washed into the Great Lakes for many years, these lakes are now one of the major sources of atmospheric PCBs. PCBs bound to dust particles have been carried over the globe by atmospheric circulation and are present in wildlife from the Antarctic to isolated Paci®c atolls. Their atmospheric concentrations are highest near urban centers in the United States and Europe, where they are present in higher quantities than in rural areas.

8.7.2 Toxicity Early concerns regarding the toxicity of PCBs were fueled by the ``Yusho incident'' in Japan in 1968, when more than a thousand persons ate rice oil contaminated with PCBs that had leaked from a heat exchanger used to process the rice oil. Persons who ate 0.5 g or more (average consumption was 2 g) developed darkened skin, eye damage, and severe acne. It is not certain whether the subsequent deaths of some of the patients were due to the PCB poisoning. Recovery was slow, with symptoms still present after three years. Several infants were born with the same symptoms, demonstrating that PCBs can readily cross

246

8.7 POLYCHLORINATED AND POLYBROMINATED BIPHENYLS

the placental barrier. Similar effects were observed on Taiwan in 1979, when cooking oil contaminated with PCBs was used by many people. While the concentration of PCBs in lakes, rivers, and oceans is low because of the compounds' low solubility in water, concentrations in animals that feed almost exclusively on ®sh can build up to 100 million times the concentration in water. Animals at the end of a food chain, such as those that eat ®sh, consume vast amounts of ®sh in their lifetimes, with the result that even though an individual ®sh may contain a low level of PCBs, the cumulative amount consumed is very large. The PCBs remain dissolved in the livers and other fatty tissues of these animals because they are so insoluble in water and because they are degraded very slowly by cytochrome P-450 in the liver. For example, herring gulls, eagles, bottlenose dolphins, seals, killer whales, and beluga whales all have been found to contain high levels (from 10 to > 200 ppm) of PCBs. The normal PCB concentration in humans is 1±2 ppm. It is known that mink are very sensitive to PCBs; only 5 ppm causes complete reproductive failure. In contrast, there is little decrease in survival of offspring in rats containing 100 ppm. There have been several episodes of chicken poisoning by feed containing PCBs. As little as 10±20 ppm causes enlarged livers, kidney damage, decreased egg production, and decreased hatchability of the eggs produced, as well as developmental defects in the chicks that do hatch. Similar effects have been observed in the birds living on the shores of the Great Lakes. Some species of shell®sh, shrimp, and ®sh also exhibit sensitivity to PCBs. There is also some concern that chronic toxic effects may occur in the animals at the end of food chains that contain high levels of PCBs. It is dif®cult to assign such effects unambiguously to PCBs because the animals also contain other stable chloroorganics in their fatty tissues. In addition, the biological effects vary with the degree of chlorination of the biphenyls and with the polychlorinated benzofuran [see Section 8.7.3, reaction (8-30)] content of the PCBs. Nor is it clear that all the toxic effects observed in humans who ingested PCB-containing cooking oil in Japan and Taiwan were due to the PCBs, since chlorobenzofurans present might have been implicated as well. PCBs and benzofurans have environmental half-lives of about 15 years, so signi®cant amounts will be in the environment well into the twenty-®rst century. It was reported in 2000 that PCBs and their dioxin and benzofuran impurities may inhibit the development of children. The study showed that young breast-fed children appear to have a weakened immune system in comparison to those fed formulas. The mothers' milk contained PCBs, while the formulas did not. The effect on the children's immune systems was small, but the breastfed children were eight times more likely to get chicken pox and three times more likely to have at least six ear infections. This study will have to be con®rmed by independent investigators before the conclusions can be generally accepted.

247

8. HALOORGANICS AND PESTICIDES

8.7.2.1 Polybrominated Biphenyls (PBBs)

Polybrominated biphenyls, ®rst sold commercially in 1970, were produced in much smaller amounts (5  106 lb.=year) than PCBs. They were used as ¯ame-retardant and ®re proo®ng materials in the polymers in typewriters, calculators, televisions receivers, radios, and other appliances. Their chemical properties are similar to those of PCBs in that they are very stable. They are an environmental problem in the Pine River, in St. Louis, Michigan, where about a quarter-pound was spilled daily during manufacture. Their deleterious effect to livestock and fowl was observed in 1973 when PBBs, sold under the commercial name Firemaster, were mistakenly substituted for Nutrimaster, a dairy feed supplement, in animal feed. Animals fed PBBs were not ®t for human consumption, and 20,000 cattle, pigs, and sheep had to be destroyed along with 1.5 million domestic fowl. The PBBs caused weight loss, decreased milk production, hair loss, abnormal hoof growth, abortions, and stillbirths. The manufacture of PBBs in the United States was banned in 1977.

8.7.3 Chemical Synthesis and Reactivity PCBs are manufactured by the direct chlorination of biphenyl in the presence of Fe or FeCl3, as shown earlier in reaction (8-11). A mixture of isomeric products is obtained, the structures of which depend on the reaction temperature and the ratio of Cl2 to biphenyl. Since the biphenyl is usually contaminated with polyphenyls such as tetraphenyl, the chloro derivatives of these products are also obtained in reactions analogous to (8-11). PCBs are among the most persistent compounds in the environment. As noted previously, they are resistant to both hydrolysis and oxidation and, as we discuss shortly, undergo slow microbial degradation. It is not surprising that biphenyls are so stable, since the aryl halide functional group is exceedingly resistant to hydrolysis (see Section 8.3.2.3). Highly chlorinated PCBs are photodegraded with the long-wavelength UV light (> 290 nm), which is not absorbed by the ozone layer. The initial step in the photodegradation process involves the dissociation of a chlorine atom, and the radicals that form abstract a hydrogen atom from another organic molecule, as shown in reactions (8-27) and (8-28). When the photolysis proceeds in the presence of water, phenols are obtained as products [reaction (8-29)] by the reaction of water with the triplet excited state of the PCB. Cl

hu

Cl

8-27

248

8.7 POLYCHLORINATED AND POLYBROMINATED BIPHENYLS

H

RH

R

8-28

* Cl

hu

Cl

H2O

8-29

OH

HCl

Photochemical reactions are not a major pathway for the environmental destruction of PCBs because only the highly chlorinated derivatives absorb at wavelengths greater than 290 nm and the quantum ef®ciency of the reactions is low. Lightly chlorinated biphenyls are not degraded photochemically in the environment because they do not absorb light at wavelengths greater the 290 nm; they absorb at the shorter wavelengths, which do not penetrate the ozone layer. PCBs have low water solubility ( 50 ppb for tetrachlorobiphenyls and 1 ppb for hexachlorobiphenyls) and are more dense than water. When discharged into lakes and rivers they sink to the bottom, where they are adsorbed on hydrophobic organic sediments. PCBs, as noted earlier, have low volatility (104 ±1011 atm), with the largest amounts in the atmospheres of urban areas (0.2±20 ng=m3 ) and the lowest in marine air (0.02±0.34 ng=m3 ). The atmospheric reservoir of PCBs is less than 0.1% of the total amount in the environment. In spite of these low volatilities, atmospheric transport is the principal way PCBs are spread globally as a gas or bound to particles. The Great Lakes of North America have become a major source of atmospheric PCBs owing to the revolatilization of the PCBs present there. PCB concentrations are high in urban areas as a result of their volatilization from municipal land®lls and waste disposal sites, where they were dumped prior to 1978, when their disposal was regulated. The destructive disposal of PCBs requires extreme reaction conditions because they are such stable compounds. Since they are resistant to air oxidation at temperatures below 7008C, incineration at lower temperatures, for example, while burning trash, results in partial oxidation to chlorobenzofurans: Cl

Cl

Cl

Cl

Cl

O2

Cl

Cl

Cl

8-30 Cl

O

Cl A polychlorinated dibenzofuran

8. HALOORGANICS AND PESTICIDES

249

Reductive removal of the chloro groups proceeds with strong reducing agents such as LiAlH4 , sodium, or titanium(III), or by catalytic hydrogenation to generate biphenyl, a compound that can be oxidatively destroyed by combustion. Complete hydrolysis can be attained by treatment with NaOH in methanol at 300±3208C and pressure of 180 kg=cm2 . High-temperature combustion ( 10008C) is used most frequently for complete destruction (> 99.9999% of the PCBs can be destroyed). Cement kilns, with their high temperatures (15008C) and basic conditions, are ideal sites for the combustion of PCBs. In this process a slurry of crushed limestone and silicate-containing rock, containing 30±40% water, is fed in one end of a 500ft rotating tube, and this slurry slowly migrates by gravity to the other end of the tube, where oil or coal and the PCBs are burning to give the high temperature. The PCBs are pyrolyzed and oxidized to carbon dioxide while burning, and the chlorine is released as HCl. The HCl reacts with the basic compounds present in the limestone to form calcium and magnesium chloride as it passes through the cement and slurry. Cement formation is a slow process, so the PCBs have a long residence time in the kiln where the temperatures are maintained at 1370±14508C in the presence of molecular oxygen. Almost all of the PCBs are destroyed, and the only emissions of chlorinated compounds observed are those detected when no PCBs were added to the kiln.

8.7.4 Microbial Degradation Soil samples containing PCBs have been found to contain microorganisms that metabolize the PCBs. Different degradative pathways have been observed which proceed in the presence and absence of molecular oxygen. 8.7.4.1 Aerobic Biodegradation

A variety of microbial types, most of which are members of the genus Pseudomonas, degrade PCBs in the presence of oxygen. They attack the more lightly chlorinated PCBs (mono- to tetrachlorinated) to give phenolic products by a pathway that is similar to the microbial oxidation of nonchlorinated aromatic compounds. The metabolic pathways used by these diverse microorganisms for PCB destruction are similar (Figure 8-3). This suggests that the degradation is catalyzed by the same group of enzymes and thus has the same genetic basis in all the microorganisms. Since it is unlikely that the same degradative pathway evolved separately in each genetic type, it appears likely that these unrelated microorganisms obtained the ability to degrade PCBs by gene transfer. These mobile genes have made it possible for microorganisms living in the presence of PCBs to gain a selective advantage over the others by utilizing the energy and carbon present in PCBs for their own metabolic processes.

250

8.7 POLYCHLORINATED AND POLYBROMINATED BIPHENYLS

OH

bphA

Clx

Clx

OH

OH

OH

H H

COOH O

OH bphB

Clx

bphC

bphD

Clx

COOH

Clx

FIGURE 8-3 Degradation of biphenyl (bph) and chlorobiphenyls (clx) by the 2,3-dioxygenase pathway in Pseudomonas strain LB400. Redrawn from F. J. Mondello, J. Bacteriol.,

, 1725 (1989). Used by permission of the American Society for Microbiology.

The genes encoding the enzymes responsible for the aerobic degradation of PCBs have been isolated, cloned, and incorporated into microorganisms such as E. coli. These genetically engineered microorganisms have the same ability to degrade lightly chlorinated PCBs as the ones found in the soil samples. It may be possible to design microorganisms that degrade PCB's faster than those that occur naturally.

8.7.4.2 Anaerobic Biodegradation

The bulk of the PCBs present in the environment are present in the sediments of lakes, rivers, and oceans where there is little or no oxygen. In some lakes, like Lake Ontario, where there is little homogenization of sediments, there are close correlations between the U.S. sales of PCBs and the concentrations of PCBs in sediment cores (Figure 8-4). Since sediments are the principal repository for PCBs, anaerobic degradative pathways are likely to be of greater importance than aerobic ones. Studies of the degradation of PCBs in the sediments of the Hudson River in New York resulted in the discovery of microorganisms that degrade PCBs in the absence of oxygen. These microorganisms degrade the more highly chlorinated PCBs (> tetrachloro) to the mono-, di-, and trisubstituted isomers. This reductive dehalogenation results in the substitution of a hydrogen for the chloro group on the aromatic ring. Similar reductive dechlorinations have been observed in the environment with other chlorinated aromatic compounds, as shown earlier in reaction (8-23). Anaerobic microorganisms reduce the chloro groups from the highly substituted biphenyls to give lightly chlorinated biphenyls, and the aerobic microorganisms destroy the lightly substituted biphenyls. In one proposed bioremediation procedure, PCB-containing soil is

251

8. HALOORGANICS AND PESTICIDES

+

PCBs 30

PCB sales in U.S. (+) (× 109g)

Accumulation (ng/cm2 yr)

40

+ +

20

+ +

+

10

1980

1970

1960

1950

1940

FIGURE 8-4 Correlation of PCBs in Lake Ontarico core samples with PCB sales in the United States: E-30 (triangles) and C-32 (circles) are cores from two different sites in Lake Ontario. Redrawn from D. L. Swockhamer and S. J. Ehrenreich, in Organic Contaminonts in the Environment. Environmental Pathways and Effects, K. C. Jones, ed., Elsevier Applied Science, London. Copyright # 1991.

to be incubated ®rst with anaerobic microorganisms in the absence of oxygen and then with aerobes in the presence of oxygen. This should result in the destruction of the PCBs in sediments, while requiring a minimal energy input to the process.

8.8 DDT AND ITS DEGRADATION PRODUCTS The insecticidal effects of DDT were discovered by the Swiss chemist Paul MuÈller in 1940, and DDT was used extensively in World War II for the control of diseases spread by ¯ies, mosquitoes, and other insects. Initially, it was very effective in killing the mosquitoes that carry the microorganism responsible for malaria. It was used directly on humans to control head lice without apparent toxic effects. In 1948 MuÈller was awarded the Nobel Prize in chemistry for his discovery.4 DDT was used in even greater amounts in the 1950s and 1960s to control insects that attack crops, in addition to its use for ¯y and mosquito control. There was a general feeling at that time that we would be able to conquer all insect pests with DDT and other pesticides.

4

The initial bene®cial effects of DDT are described in M. Gladwell, ``The Mosquito Killer,'' The New Yorker, July 2, 2001, pp. 42±51.

252

8.8 DDT AND ITS DEGRADATION PRODUCTS

8.8.1 Synthesis DDT [1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane] (also called dichlorodiphenyltrichloromethane, hence DDT), is prepared by reaction (8-31) between trichloroacetaldehyde (chloral) and chlorobenzene. The mechanism of the reaction involves the electrophilic addition of a carbocation to the aromatic ring; a Friedel±Crafts type of reaction. The mechanism is shown in reactions (8-31)±(8-34). Cl CCl3 H

CCl3CHO

Cl

CH

8-31

Cl

p, p'- DDT

OH H

CCl3CHO

8-32

CCl3CH

Cl CCl3

OH Cl

CCl3CH

CH

8-33 H2O

CCl3 Cl

CH

Cl

8-34

CCl3 Cl

C

Cl

H

H

The p,p -isomer shown in reaction (8-31) is not the only reaction product. Appreciable amounts of o,p - and o,o -DDT are also obtained. This synthetic approach has been applied for the preparation of a great variety of DDT analogues. One important example, methoxychlor, is used in place of DDT in many applications because it is biodegradable. CCl3 CH3O

CCl3CHO

H

CH3O

C H Methoxychlor

OCH3

8-35

253

8. HALOORGANICS AND PESTICIDES

Methoxychlor in less effective as an insecticide, however, and about three times as costly to prepare, since anisole (methoxybenzene) is a more expensive starting material than chlorobenzene. The estimated LD50 (lethal dose for 50% of the population) of methoxychlor in rats is 5000±7000 mg=kg (VS 250± 500 mg=kg for DDT).

8.8.2 Environmental Degradation The ®rst step in the degradation of DDT is the relatively rapid elimination of HCl to form DDE (1,1-dichloro-2,2-bis(p-chlorophenyl)ethylene) (reaction 8-37) when the DDT is heated in water. However, the subsequent hydrolysis of DDE to DDA is extremely slow, as indicated in reaction (8-37), because there are only unreactive vinyl and aryl chlorides in DDE. CCl3 Cl

C H

CHCl2 Cl

Reduction

Cl

DDT

C H

Cl

8-36

DDD

Fast CO2H

Cl CCl Cl

C DDE

Cl

Slow H2 O

Cl

C H

8-37 Cl

DDA

DDD (also known as TDE), a major microbial metabolite of DDT formed by reductive dechlorination, has also been used as an insecticide (Rothane). Because of reactions (8-36) and (8-37), both DDD and DDE accompany DDT and DDA in the environment, so when the mixture of DDT and its degradation products is reported in environmental samples, it is often referred to as DDT. Methoxychlor and other DDT analogues that do not contain the p,p -chloro group are much less persistent than DDT in the environment. This is due to their metabolism by soil microorganisms to phenols that are readily degraded to acetate in accordance with reactions (8-38) and (8-39). o,p-DDT (8-38) is known to have estrogenic activity (Section 8.5.1).

254

8.8 DDT AND ITS DEGRADATION PRODUCTS

CCl3 Cl

C H Cl o,p′-DDT

8-38

CCl3 Cl

C H

OH

Further degradation

Cl CCl3 CH3O

C H

OCH3

Methoxychlor HO

8-39 CCl3 C H

OCH3

Further degradation

The enzymes involved in these oxidations are probably of the cytochrome P-450 type mentioned earlier (Section 8.5). Cytochrome P-450 enzymes are also present in insects. The lower toxicity of methoxychlor (vs DDT) may re¯ect the effective oxidative detoxi®cation of methoxychlor by some insects.

8.8.3 Mechanism of Action of DDT and DDT Analogues as Pesticides Insects sprayed with DDT exhibit hyperactivity and convulsions consistent with the disruption of the nervous system by DDT. Many theories have been suggested for the toxic effect of DDT, and the exact mechanism is not known. A theory that appears to be plausible and has some experimental basis suggests that the DDT molecules are of the correct size to be trapped in the pores of the nerve membranes, which are thus distorted, allowing sodium ions to leak through and depolarize the nerve cell so that it can no longer transmit impulses. This theory states that the toxicity of DDT is not due to its chemical reactivity but rather to its size and geometry, which allow for the blockage of the pores of the nerve membranes. This theory is supported by the observation that a variety of quite different compounds that are stereochemically similar to DDT exhibit DDT-like activity. This ``special ®t'' hypothesis is supported by the observation that the biological activity of methoxychlor analogues decreases rapidly when R in the following formula contains ®ve carbon atoms or more.

255

8. HALOORGANICS AND PESTICIDES

CCl3 RO

C H

OR

Methoxychlor analogue; R is substituted for CH3

Presumably the longer chain methoxychlor analogues are not able to ®t into the nerve pores. Insects are especially susceptible to DDT because it is readily absorbed through the insect cuticle. DDT is not appreciably absorbed through the protein skin of mammals and does not exhibit acute toxicity. This is why it could be safely applied directly to humans to kill head lice. If the polarity of the DDT analogue is increased by introducing NO2 , CO2 H, CO2 CH3 , and OH substituents into the aromatic ring, the toxicity to insects is lost. This loss is probably due in part to decreased absorption through the exoskeleton and in part to decreased adsorption on the nonpolar nerve membrane.

8.8.4 Chronic Toxicity of DDT and Related Compounds The large-scale use of DDT as an insecticide entailed the release of large amounts into the environment, where it and its degradation products persist for decades. These compounds are so volatile that, like PCBs, they were spread worldwide in small amounts by the global winds. Yet while the use of DDT was increasing, it was noted that there was a decrease in many species, especially those at the end of food chains, on earth. These included especially eagles, hawks, and falcons, birds that feed mainly on ®sh. Correlations were observed between the decreasing number of young hatched and the amounts of DDT and its degradation products in the eggs that did not hatch. A greater number of broken eggs than usual were found in the nests, and all the eggs, both whole and broken, had thinner shells than normal. In addition, the adults tended to mate later than usual in the summer, giving their progeny less time to mature before winter arrived. Thus fewer of the immature adults survived to have offspring the following summer. All these factors resulted in a precipitous drop in the populations of these ®sh-eating birds. The presence of both DDT and its degradation products and PCBs in the eggs that did not hatch suggested that both chloroorganics may have been responsible for the collapse of the populations of these birds. In the United States, the manufacture and use of DDT was stopped in 1972, and the manufacture of PCBs was halted in 1977. Within 10 years after the DDT ban, there was a marked increase in the number of young hatched by the affected birds and a corresponding decrease in the amounts of DDT and its degradation products in the eggs that did not hatch. In addition, there was a corresponding

256

8.8 DDT AND ITS DEGRADATION PRODUCTS

increase in the thickness of the egg shells. During this time period there was no change in the levels of PCBs in the eggs, suggesting that DDT and its derivatives were responsible for the initial decrease in these bird populations. Independent studies have shown that low concentrations of PCBs have little effect on the thickness of avian eggshells. There are two proposals to explain the connection between eggshell thickness, mating behavior, and the DDT. In one theory the connector is the monooxygenase enzyme cytochrome P-450. As noted in Section 8.5, high levels of liver cytochrome P-450 are induced by some chlorinated organics, levels that remain high if the chloroorganics are heavily chlorinated and thus dif®cult to oxidize. DDT residues induce cytochrome P-450 isozymes, structurally different P-450s which have similar catalytic activity and cause changes in the level of the steroid hormone estradiol, which controls mating behavior. OH CH3

HO Estradiol

The production of eggshells is also in¯uenced by estradiol. The shell of an egg is not formed until the last day before laying. About 60% of the calcium needed to form the egg is obtained from the bird's food intake, and the remainder comes from calcium stored in bones. Since the level of calcium deposited in the bones is regulated by levels of estradiol in the blood, a low level of estradiol results in a low level of stored calcium. The absence of stored calcium could be a signi®cant factor in egg survival, since a 20% decrease in shell thickness results in extensive egg breakage. A 20% decrease in shell thickness is correlated with as little as 25 ppm DDT or its breakdown products observed in the egg. In addition, it has been observed that some pesticides inhibit the formation of eggshells even in the presence of an adequate supply of calcium. Presumably these pesticides interfere with the enzyme carbonic anhydrase, which is responsible for the conversion of carbon dioxide to carbonate. The latter is required to combine with calcium to form the calcium carbonate of the shell. It has been established that DDE interferes with the formation of the shell in this way. The connector between DDT, DDE, and thin eggshell and delayed mating of birds in the second proposal is the induction of hyperthyroidism in birds. This proposal has been questioned by Moriarity.5 It has been observed that when 5

F. Moriarity, ed., Organochlorine Insecticides: Persistent Organic Pollutants. Academic Press, New York, 1975.

257

8. HALOORGANICS AND PESTICIDES

1.3

130

1.0

100

0.7

70

0.4

40

DDT ban

0.1

1966

1968

1970

1972

1974 Year

DDE (ppm, dry weight) ( )

Mean number of young per breeding area (•)

these chemicals are administered to some strains of birds, there is a doubling of the size of the thyroid gland. Increased metabolism, pulse, and heart size are indicative of hyperthyroidism. Studies on birds with hyperthyroidism have shown that they delay mating, and lay lighter eggs with thinner shells. Male birds with hyperthyroidism have signi®cantly lower fertility than those that do not. It is not clear at the time of writing if either of these proposals is correct or whether there is yet another explanation for the biological effects of DDT and its degradation products on fowl. After DDT was banned, its levels in the environment slowly decreased over a 10-year period (the half-life of pure DDT is about 10 years, but its degradation products last much longer), and consequently its levels in ®sh and the animals that consumed the ®sh also decreased, and the steroidal hormonal balance gradually swung back closer to the pre-DDT levels. The result of the ban is that most of the eagles, hawks, pelicans, and falcons in the lower 48 states of the United States have returned to close to their pre-DDT levels either naturally or, in the case of some eagles, with the help of their reintroduction from Alaska and Canada (Figure 8-5). Another example is the dramatic

10

1976

1978

1980

FIGURE 8-5 Summary of average annual bald eagle reproduction and DDE residues in addled (spoiled) eggs in north western Ontario, 1966±1981. Dashed lines indicate weighted mean concentrations of DDE residues in clutches before (94 ppm) and after (29 ppm) the ban of DDT. Means for the 16-year period are 57 ppm DDE (weighted mean) and 0.82 young per breeding area. Redrawn with permission from James W. Grier, Science,
1232±1236. Copyright # 1982 American Association for the Advancement of Science.

258

8.9 OTHER CHLOROORGANIC PESTICIDES

TABLE 8-3 Brown Pelican Breeding in Coastal Southern California (U.S.) and Northern Baja California (Mexico) and the Content of DDT and Its Breakdown Products in Anchovies and Pelican Eggs DDE, DDT, and DDDa

Year

Nests built

1969 1970 1971 1972 1973 1974

1125 727 650 511 597 1286

Anchovies Young ¯edged (ppm, fresh wet weight)b 4 5 42 207 134 1185

4.27 1.40 1.34 1.12 0.29 0.15

Pelican eggs (ppm, lipid mass)c 1055

>221 183 97

a About b

95% DDE. A major food for the brown pelican. c Addled and broken eggs. Source: Adapted from D. W. Anderson, R. W. Risebrough, L. A. Woods, Jr., L. R. Deweese, and W. G. Edgecomb, Brown pelican: Improved reproduction of the southern California coast, Science, 190, 806±808 (1975).

increase in the successful hatching of the brown pelican after 1970, when ef¯uent from a DDT manufacturing facility in Los Angles was diverted from the Paci®c Ocean to a land®ll (Table 8-3). Although the manufacture and use of DDT has been banned in Europe and North America, it is still used in large amounts in India, Africa, the Middle East, Southeast Asia, and Central and South America. One of its major uses is for the control of the anopheles mosquito, which transmits malaria to humans. The total DDT use in developing countries at the turn of the century was comparable to that used in the developed countries in the 1960s. The volatility and stability of DDT and its degradation products, which have an approximate half-life of 60 years in temperate climates, suggests that these compounds will continue to be an environmental problem for many more years unless all the nations of the world decide to ban the manufacture and use of the pesticide. 8.9 OTHER CHLOROORGANIC PESTICIDES 8.9.1 Lindane 8.9.1.1 Synthesis

Lindane, the g-isomer of 1,2,3,4,5,6-hexachlorocyclohexane, is prepared by the photochemical initiated addition of chlorine to benzene, as shown in reaction (8-40).

259

8. HALOORGANICS AND PESTICIDES

Cl a

Cl

Cl

Cl

Cl

Cl

+

Cl

Cl a Cl α (aaeeee) (53–70%)

Cl

+ Cl2

hu

Cl Cl

Cl

Cl

Cl

+

Cl

Cl β (eeeeee) (3–14%)

8-40

Cl

Cl +

Cl

Cl Cl γ (aaaeee) (11–18%) (Lindane)

Cl

Cl

δ (aeeeee) (6–10%)

In this reaction four of the eight possible isomers of 1,2,3,4,5,6-hexachlorocyclohexane, are formed in appreciable amounts. These isomers differ in the relative orientations of the chloro substituents. Axial (a) groups are perpendicular to the cyclohexane ring and are labeled in the a-isomer in reaction (840). Equatorial groups are in the equatorial plane of the ring as shown in the b-isomer. Only one of these isomers, the g-isomer, exhibits signi®cant insecticidal action. Initially, the total reaction mixture was used as the insecticide. However, that practice was discontinued because it resulted in the distribution into the environment of large amounts of potentially toxic chlorocarbon compounds, which do not have insecticidal activity. Initially the use of lindane was banned in the United States, but that ban was lifted, and it is now imported for some speci®c uses. For example, lindane is used as a soil insecticide and on cotton and forest crops. Lindane is excreted rapidly, and its acute mammalian toxicity is low. The b-isomer tends to accumulate in mammalian tissues and exhibits chronic toxicity. The volatility of the g-isomer is high, which makes it useful as a soil insecticide, but this volatility results in its distribution far from the point of use. 1,2,3,4,5,6-Hexachlorocyclohexane accumulates in plankton and ®sh (presumably the b-isomer), along with DDT residues and PCBs, with the highest concentrations being found in bottlenose dolphins and other animals at the end of the food chain.

260

8.9 OTHER CHLOROORGANIC PESTICIDES

8.9.1.2 Environmental Degradation

Lindane is an inert chloroorganic that undergoes a very slow elimination of HCl in aqueous solution in path (a) of reaction (8-41). Presumably this is an E1 reaction [see reactions (8-14) and (8-17)]. Lindane is also degraded by microorganisms by a combination of reductive and elimination pathways to 1,2,4trichorobenzene [see path (b) of reaction (8-41)]. Cl Cl Cl Cl

H 2O

Cl

Cl

Cl

(a)

Cl

Cl

microorganisms

Cl

8-41 Cl

Cl

(b)

Cl

(and other isomers) Cl

8.9.2 Polychlorinated Cyclodienes 8.9.2.1 Synthesis

A series of bicyclic insecticides, mirex, chlordane, heptachlor, aldrin, and dieldrin, can be synthesized by the Diels±Alder addition of hexachlorocyclopentadiene to ole®ns, as follows: Cl

Cl

Cl

Cl Cl2

+ Cl2

Cl Cl

350–500⬚C

Cl

Cl Cl

+ HCl

8-42

Cl hexachlorocyclopentadiene

The preparation of these compounds is shown in reactions (8-43) and (8-44). It is possible to use the Diels±Alder reaction to prepare a whole series of potential insecticides simply by varying the diene and ole®n.

261

8. HALOORGANICS AND PESTICIDES

Cl

Cl Cl Cl Cl

Cl

Cl

Cl

Cl + Cl

Cl

Cl Cl2

(a)

SO2Cl2 (a source of Cl)

(b)

Cl

Cl

Cl

Cl Cl

Cl

8-43

Cl

Cl Cl

Cl

Cl

Cl

Chlordane

Cl

Cl Heptachlor

Cl

Cl Cl Cl Cl

Cl

+

Cl

Cl

Cl

Cl

Cl

Cl

Cl

8-44 Cl

Cl

H2O2

Cl

Cl

Cl

Cl O

Aldrin

Dieldrin

Mirex, another insecticide, is prepared by the aluminum chloride catalyzed cyclodimerization of hexachlorocyclohexadiene, as in reaction (8-45). It is one of the most stable known organic compounds and has a melting point of 4858C.

262

8.9 OTHER CHLOROORGANIC PESTICIDES

Cl

Cl Cl

Cl

Cl

Cl Cl

Cl

Cl Cl

AlCl3

Cl

Cl

Cl Cl

Cl Cl

Cl

Cl Cl

8-45

Cl

Cl

Cl

Cl

Cl

Mirex

H H

8-46

Endo (predominant product)

8-47 Exo (minor product)

The endo adduct shown in reaction (8-46) is the major product resulting from the Diels±Alder addition of a diene and an ole®n. No intermediate has been detected, but the reaction product can be rationalized as having originated from a transition state in which there is maximum interaction between the p bonds of the ole®n and diene. This is illustrated in reactions (8-46) and (8-47), in which the upper cyclopentadiene may be regarded as the ole®n, and the lower cyclopentadiene, the diene. 8.9.2.2 Environmental Degradation

The cyclodiene insecticides are very resistant to environmental degradation. One might expect that the tertiary, allylic chloro groups at the bridgehead carbons would be especially susceptible to SN 1 hydrolysis or E1 elimination [see reaction (8-14)]. However, the rigid geometry of the bicyclic ring system prevents carbocation formation, as shown in reaction (8-48).

263

8. HALOORGANICS AND PESTICIDES

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl Cl

Cl

Cl

+

8-48

Cl

Cl Cl

Cl

A carbocation is more stable if the positive central carbon atom and the three substituents attached to it are in the same plane. It is not possible to obtain a planar carbocation intermediate at the bridgehead carbon atom of these compounds without introducing extraordinary strain in the bicyclic system. Consequently, the chloro groups at the bridgehead position are quite unreactive. Some of the cyclodiene insecticides are susceptible to oxidative attack by soil microorganisms, plants, and animals, and by UV. However, the resulting products, such as the one illustrated in reaction (8-49), are often more toxic than the starting pesticide. Cl

Cl

Cl

Cl Heptachlor

8-49 Cl

Cl

O Cl

Photodieldrin, shown in reaction (8-50), is formed by the action of ultraviolet light (UV-B, 290±320 nm) as well as by the action of oxidase enzymes on Dieldrin. The photoproduct of heptachlor is more resistant to environmental degradation than heptachlor itself. Cl

Cl

Cl

Cl Aldrin

Dieldrin

8-50 Cl

Cl Photodieldrin

O

264

8.9 OTHER CHLOROORGANIC PESTICIDES

Aldrin, dieldrin, heptachlor, and chlordane have been used to kill grubs and other soil pests and were applied mainly to corn and cotton. Dieldrin has also been used to control the anopheles mosquito. The mechanism of action of these bicyclic organochlorine compounds is similar to that of DDT. However, their toxic effects as insecticides suggest that the site of action lies in the ganglia of the central nervous system rather than the peripheral nerves that are affected by DDT. Mirex has a long lifetime in the environment and a half-life in mammals of about 10 years. It was used extensively in the southern United States in the 1950s and 1960s in an attempt to control the ®re ant, an accidentally introduced species from South America. Fire ants live in large colonies in mounds they construct in pasture land. Humans and livestock that step in the mounds are aggressively attacked and bitten by hordes of ®re ants coming out of the mound. At one point attempts were made to control the ®re ants by using World War II bombers to drop a mix of ant food and mirex on pastures. This killed not only the ®re ants but also all the other ants and many other insects as well. When the plan failed to eradicate the ®re ant, the Mirex treatment was terminated. Since the ®re ant has a more ef®cient mechanism of recovery than the indigenous ants, it took over the ®elds that had been treated with Mirex when the pesticide was washed away. So the Mirex eradication plan actually enhanced the spread of the ®re ant by killing the indigenous ants that were the barrier to its rapid spread throughout the South. Because of their potential danger as carcinogens and because they accumulate in fatty tissues of birds and mammals, the Environmental Protection Agency has terminated the use of mirex (1971), aldrin and dieldrin (1974), and heptachlor and chlordane (1976). Exemptions for use in special instances have been granted. An example of an exemption gone bad resulted in the contamination of milk in Hawaii, where a request for the use of heptachlor to control aphids (mealybugs) on pineapple plants in was granted in 1978. The aphids cause ``mealybug wilt,'' which withers pineapple roots. The aphids are carried to the pineapple plants by ants which, in return, collect the ``honeydew'' produced by the aphids. The aphids were controlled by killing the ants with Heptachlor. At the same time heptachlor was being used, agricultural scientists were working on a procedure to use pineapple plants, after the pineapples had been harvested, as cattle feed. The plants were not supposed to be fed to cattle until one year after the last application of heptachlor, but in 1982 this procedure was not followed. Consequently, high concentrations of the hydrophobic heptachlor ended up in the milk of the cows that were fed the pineapple plants, and the contaminant was passed on to those drinking the milk, mainly children. These high levels were detected in the semiannual screening of pesticides in milk by the Hawaii Health Department.

265

8. HALOORGANICS AND PESTICIDES

8.10 HERBICIDES: 2,4-DICHLOROPHENOXYACETIC ACID AND 2,4,5-TRICHLOROPHENOXYACETIC ACID 8.10.1 Introduction 2,4-Dichlorophenoxyacetic acid (2,4,-D) and 2,4,5-triphenoxyacetic acid (2,4,5-T) are herbicides that are especially effective in the control of broadleafed plants, yet they have little or no effect on grasses. Hence they are used to control weeds and other unwanted vegetation where only grasses are desired. These compounds mimic the plant growth hormone (auxin) indoleacetic acid. CH2CO2H

N H Indoleacetic acid

However, the large amounts used (in comparison to the natural auxin) cause abnormal growth and eventual death of the plant. Speci®c results include little or no root growth, abnormal stem growth, and leaves with little or no chlorophyll. 8.10.2 Synthesis 2,4-D and 2,4,5-T are manufactured by the SN 2 displacement of the chloro group of chloroacetate with a phenoxide anion as in reactions (8-51) and (8-52) or by the chlorination of phenoxyacetic acid, as in reaction (8-53). _

_

ONa+ + ClCH2CO2

Cl

_

+

OCH2CO2 Na

Cl

8-51

Cl

Cl

2,4-D

Cl

Cl _

_

ONa+ + ClCH2CO2

Cl Cl

_

Cl

+

OCH2CO2 Na Cl 2,4,5-T

8-52

266

8.10 HERBICIDES

−

+

OCH2CO2 Na

_

OCH2CO2 Na+

Cl

+ Cl 2

8-53 Cl 2,4-D

A variety of closely related 2,4-D analogues also show herbicidal activity. The carboxyl group can be replaced by an amide, nitrile, or ester group. In addition, a longer side chain can be used in place of the acetic acid moiety. However, this side chain must contain an even number of carbon atoms to be active. This result is consistent with b-oxidation of the side chain by the plant (Section 7.2.4) to form the biologically active 2,4,-D. Cl

b-oxidation

OCH2CH2CH2CO2H

OCH2CO2H + CH3CO2H

Cl

Cl

8-54

"Active" Cl Cl

OCH2CH2CO2H

b-oxidation

Cl

Cl "Inactive"

OH + CO2 + CH3CO2H

8-55

Cl

8.10.3 Environmental Degradation 2,4-D and 2,4,5-T are subject to rapid environmental degradation. These compounds are cleaved by microorganisms to the corresponding phenol, which is readily degraded further. Presumably, carbon dioxide and formic acid are the other reaction products: OCH2CO2H

Cl Cl

Cl

OH + CO2 + HCOOH

8-56

Cl

In addition, the photochemical cleavage of the acetic acid side chain and the photochemical hydrolysis of the aryl chloro groups have been demonstrated. These ®ndings suggest that the long-term environmental impact of these compounds is small.

267

8. HALOORGANICS AND PESTICIDES

The environmental problem that has been associated with these compounds is due to 2,3,7,8-tetrachlorodibenzo-p-dioxin (TCDD) impurities produced during their manufacture. The synthesis of 2,4-dichlorophenol and 2,4,5-trichlorophenol (8-57) results in the formation of small amounts of TCDD (8-58), which are carried along with the ®nal product. Cl

Cl

Cl

OH

Cl

Cl

NaOH

Cl

Cl

high pressure and temperature

8-57

2,4,5-Trichlorophenol

Cl

O–

Cl

Cl

Cl

Cl

Cl

Cl

Cl

Cl

O

Cl

Cl

Cl

Cl NaOH

Cl

O

Cl

Cl

Cl

O

Cl

Cl

O

O-

8-58

Cl

Cl

Cl

2,3,7,8-Tetrachlorodibenzo-p-dioxin (TCDD)

TCDD is formed because of the vigorous conditions that are required to hydrolyze the aryl chloro groups. The presence of TCDD in 2,4,5-T led to the ban of its use in the United States in 1979. Related toxic ®ve-membered ring derivatives [polychlorinated dibenzofurans: reaction (8-30)], formed in the manufacture of PCBs, may be also responsible for some of the toxicity of these compounds. It is generally considered that 2,4-D is safe, but it has been established that it belongs to the class of compounds called peroxisome proliferators. Cell structures containing bundles of enzymes are called peroxisomes. Compounds that induce the formation of peroxisomes are also known to cause tumors and testicular damage in rodents. It has also been suggested as the cause of non-Hodgkins lymphomas in the Vietnam veterans who handled Agent Orange (discussed shortly) and as an immune system suppressor. TCDD and other dibenzofurans, substituted with different amounts and different patterns of substituents, as well as polychlorinated benzofurans, are formed during the incineration of municipal waste. The polychlorinated dibenzodioxins and polychlorinated dibenzofurans are present in the waste after incineration in amounts 2±100 times greater than the amounts present before

268

8.10 HERBICIDES

incineration. Their formation is not due to pyrolysis of chloroorganics [e.g., poly(vinyl chloride)] present. Rather, it has been established that the polychlorinated dibenzofurans and polychlorinated dibenzodioxins are synthesized from the carbon and chlorine formed in the combustion process in reactions catalyzed by the ¯y ash formed at 250± 4008C in the postcombustion zone in the incinerator. Fly ash is the ®ne particulate inorganic material formed from the inorganics that constitute about 25% of municipal waste. This ash consists of an array of metal salts, any of which could serve as a catalyst for the synthesis of TCDDs and polychlorinated benzofurans. Isotope labeling studies have shown that these compounds form directly from carbon or from the chlorinated phenols that are produced in the combustion process. The level of the toxicity of TCDD (Section 8.7.2) varies dramatically in animals, and it is not possible to estimate its toxicity to humans (Table 8-4). It was listed as ``known to be a human carcinogen'' by the U.S. National Toxicity Program in January 2001. The toxicity to humans and a wide array of mammals was, however, demonstrated when dioxins were present in some oil applied to the soil in a horse arena in Missouri. Contact with only 32 mg of dioxins per gram of soil was suf®cient to kill the birds, cats, dogs, and horses that used the arena. Humans were less sensitive, but one child developed hemorrhagic cystitis and several other skin lesions. The acnegenic effect has been observed in workers involved in the manufacture of 2,4,5-T. Similar toxic effects were noted in 1976 when 1±4 lb of TCDD was accidentally released over a 123-acre area near the northern Italian town of Seveso. At a plant where 2,4,5-trichlorophenol was manufactured, a reactor had overheated, blowing out a plume that contained TCDD and trichlorophenol. Many animals were killed by the TCDD, but the main immediate problem

TABLE 8-4 Variation in TCDD Toxicity Animal Guinea pig Mink Rat Monkey Rabbit Mouse Dog Hamster

LD50 mg/kg 0.6±2.5 4 22±330 100± 50) organic compounds that are speci®cally regulated are not included.

426

11.5 WATER TREATMENT

TABLE 11-4 Examples of Drinking Water Standards for Inorganic Substances

Substance

U. S. Standards World Health [(mg=liter), values Organization recommendations in parentheses are recommendations] (mg=liter)


Aluminum Ammonia Antimony

0.2 1.5 0.005

Arsenic

Barium

Chloride Chlorite Chromium

(0.05±0.20)

European Union Standards (mg=liter)

0.006

0.005

0.2 0.5 0.005

0.01

0.05

0.025

0.01

0.7

2

1

Beryllium

Boron Bromate Cadmium

Canadian standards (mg=liter)

0.004

0.3 25 0.003

5 0.005

0.005

1 0.01 0.005

1.5 0.05

0.05

250 200 0.05

(250) 1.5 0.1

Copper

1

1.3 (1)

1

2

Iron Lead

0.3 0.01

(0.3) 0.015

0.3 0.01

0.2 0.01

Manganese Mercury

0.1 0.001

(0.05) 0.002

0.05 0.001

0.05 0.001

Sources in drinking water

Fire retardants, ceramics, electronics, solder, ®reworks Smelters, glass, electronics, pesticides, natural deposits Natural deposits, pigments, epoxy sealants Electrical and aerospace industries, metal re®neries, coal burning

Galvanized pipe, batteries, paint, natural deposits

Mining, electro plating, pigments, natural deposits Plumbing, wood preservatives, natural=industrial deposits Plumbing, solder, natural=industrial deposits Batteries, electrical equipment, crop runoff, natural deposits (  )

427

11. WATER SYSTEMS AND WATER TREATMENT

TABLE 11-4 (  )

Substance

World Health U. S. Standards Organization [(mg=liter), values recommendations in parentheses are (mg=liter)
recommendations]

Canadian standards (mg=liter)

European Union Standards (mg=liter)

Molybdenum Nickel

0.07 0.02

Selenium

0.01

0.05

0.01

0.01

Silver Thallium

0.1

(0.1) 0.002

0.05

0.01

Cyanide

0.07

Fluoride

1.5

0.02

0.2

4 (2)

Nitrate

50 (as nitrate)

10 (as N)

Nitrite

3 (as nitrite) 250

1 (as N)

Sulfate Zinc

3

(250) (5)

0.2

0.05

1.5

1

10

3.2 500

50

0.5 250

Sources in drinking water

Batteries, natural deposits Mining, smelting, coal=oil combustion, natural deposits Electronics, drugs, alloys, glass Electroplating, plastics, mining, fertilizer Fertilizer, aluminum industry, water additive, natural deposits Fertilizer, animal waste, sewage= septic tanks, natural deposits As nitrate Water processing, natural sources

5




World Health Organization,       
  
  
, 2nd ed. WHO, Paris, 1993.  U. S. Environmental Protection Agency, National Primary Drinking Water Standards; available at http:==www.epa.gov=OGWDW=wot=appa.html.

From Environmental Health Laboratories data as given at http:==www.mastechnology.com=InfoPages=IntDW.html.

11.5.1 Domestic Water Treatment The typical steps in treating water for household use in the United States and many other developed countries consist of (1) settling of suspended material, (2) aeration to aid in the oxidation of easily oxidized organic matter, (3) a preliminary chlorine treatment to remove bacteria and other organic material through oxidation, (4) use of a ¯occulating agent such as alum (aluminum sulfate) to carry down particulate matter, (5) addition of lime [Ca…OH†2 ] to

428

11.5 WATER TREATMENT

Settling

Oxidation

Flocculation/ Filtration/ pH Adjustment

Disinfection

FIGURE 11-4 The common steps in the treatment of domestic water.

control pH and assist in the ¯occulation process, (6) ®ltration (through sand beds), and (7) a ®nal chlorine treatment. Activated carbon may be used in some circumstances to absorb traces of material that give odor or taste, and a ¯uoride source (e.g., Na2 SiF6 ) may be added as a dental health measure. Figure 11-4 shows a schematic block diagram of the process. Suspensions of small particles in a liquid (colloids, Section 9.6) are often stabilized by adsorption of ions on the surface of the particles; if ions of a particular charge are adsorbed preferentially, the colloidal particles will repel each other and coagulation will be impeded. Various chemicals can be used that form insoluble precipitates that carry down the suspended materials. Examples are compounds of Fe(III) and Al(III), which on hydrolysis form the insoluble hydrated oxides discussed in Chapter 10. As mentioned earlier, aluminum sulfate, Al2 …SO4 †3 , is a widely used chemical for water treatment. Ferrous sulfate is another; it is oxidized by oxygen in the water to ferric ions. Hydrolysis of both Al(III) and Fe(III) produces polynuclear hydroxo species that are readily adsorbed on the surface of the suspended material, and as these hydroxo compounds further condense to insoluble forms, bind the particles with the ¯oc as it settles. If the pH is near neutrality, both Al(III) and Fe(III) are completely hydrolyzed and the added materials are completely removed from the water (see Section 10.6.3). The pH may be adjusted to ensure this by the addition of a base such as Ca…OH†2 (lime). The reaction can be summarized: Al2 …SO4 †3 ‡ 3Ca…OH†2 ! 3CaSO4 ‡ 2Al…OH†3

…11-10†

429

11. WATER SYSTEMS AND WATER TREATMENT

The small amounts of calcium and sulfate ions left in solution are not harmful. The best-known step in the treatment process for drinking water is chlorination. Chlorine is a strong oxidizing agent and in water produces hypochlorite, which is widely used in bleaches (Section 10.6.13): Cl2 ‡ 2H2 O ! Cl ‡ HOCl ‡ H3 O‡

…11-11†

This reaction is essentially complete at normal pH (the room temperature equilibrium constant is 45  10 4 mol2 =liter2 ). HOCl is a weak acid (a 3  10 8 ) and will be present as both HOCl molecules and OCl ions, with relative amounts depending on the pH. (Concentrations will be equal at pH ˆ pa ; Chapter 9.) These species are referred to as free available chlorine. The HOCl molecule is most effective as a disinfectant, presumably because it can enter bacterial cells more easily than the ion. The primary purpose of the chlorine treatment is to oxidize organic materials in the water, especially bacteria. The redox half-reaction of HOCl is HOCl ‡ H‡ ‡ 2e ! Cl ‡ H2 O;

E8 ˆ 149 V

…11-12†

Oxidizing conditions must be maintained throughout the entire distribution system to prevent redevelopment of septic conditions while ensuring that the chlorine content is not excessive near the addition point. The stability of the hypochlorite with respect to disproportionation to Cl and ClO3 is dependent on the pH, which may require adjustment for this reason, as well as to reduce the corrosive properties of the water. Although chlorination oxidizes many organic materials, it does not oxidize all. It can result in chlorination of some molecules, with the possibility of producing chlorinated hydrocarbons with signi®cant health hazards (Section 8.3.1). Chloroform is one of the potential by-products of water chlorination that is of concern. It may arise from the well-known haloform reaction, in which compounds that have structures CH3 C…O†R or CH3 CH…OH†R, or can be oxidized to form these structures (e.g., ole®ns) undergo a reaction in which the hydrogens on the carbon adjacent to the one carrying the oxygen undergo a dissociation to form the carbanion intermediate ‰CH2 C…O†RŠ followed by displacement of the Cl of HOCl to give the chlorinated product. This continues until all the hydrogens have been replaced, whereupon hydrolytic cleavage of the CÐC bond releases chloroform, CHCl3 , as illustrated in the following reaction scheme. O

O RCCH3

O

H + RCCH2 + Cl OH

O RCCCl3 + OH

OH

O RCOH +

CCl3 + H2O

+ RCCClH2

Repeat twice more

CHCl3 + OH

430

11.5 WATER TREATMENT

This reaction will occur with other halogens and is the basis of a qualitative test for the CH3 COÐ group. Phenols are another class of organic compound that can be chlorinated by HOCl. Chlorinated phenols have very noticeable, antiseptic-like odors that are detectable at the parts-per-billion range. These chlorination reactions are most expected in waters containing much industrial waste, where suitable organic molecules are present in signi®cant amounts. Of course, such waters may already contain chlorinated hydrocarbon wastes, and the extent to which chlorination actually contributes to the total is not always clear in ®eld situations. However, reactions with naturally occurring organic materials also are of concern. Humic substances (Section 9.5.7) in particular are suspected of being able to yield chlorinated products when they are present in large amounts in the water source. There are also concerns that harmful partially oxidized but not chlorinated by-products might be formed (e.g., epoxides). In the presence of ammonia, HOCl will form chloramines (e.g., monochloramine) from the reaction NH3 ‡ HOCl ! NH2 Cl ‡ H2 O

…11-13†

Under appropriate conditions, the reaction of the chlorine is fast and essentially complete, although at high chlorine=ammonia ratios or low pH values, di- and trichloramine can be formed. Analogous reactions take place with organic amines. Production of these materials may contribute to odor and taste problems in the treated water. On the other hand, combining ammonia with chlorine treatment can eliminate the formation of tastes or odors associated with the formation of chlorinated phenols, since the chloramine is a poor chlorinating agent and also gives a more persistent disinfectant action. This combined treatment (sometimes called chloramination) is used in a few public water supply treatment facilities in the United States. The chloramine slowly hydrolyzes to HOCl, prolonging the lifetime of the disinfectant, and producing it at a lower concentration so that chlorination reactions are reduced. While bromine and iodine are not used to treat public water supplies, they have been used in disinfection of swimming pools. Iodine is used to treat water that is used for drinking in wilderness treks and so on, often as tetraglycine hydroperiodide: a complex of glycine, hydriodic acid and iodine having the composition ‰NH2 CH2 COOH†16 …HI†4 …I2 †5 Š†. The chemistry of bromine resembles that of chlorine closely, but in contrast to HOCl and HOBr, HOI is not stable and decomposes rapidly to I and IO3 so that there is no residual disinfection action. While in many U.S. localities the law allows no substitute for chlorine treatment of drinking waters, an alternate method is available and receives some use in Europe and Canada, namely, treatment of the water with ozone, O3 . This method is as effective as treatment with chlorine, may have taste advantages, and avoids the risks of generating chlorinated products, although

11. WATER SYSTEMS AND WATER TREATMENT

431

the question of whether it can produce partially oxidized toxic products has been raised. There is also some concern that ozone can react with inorganic bromide to produce substances that are effective in brominating organic compounds that have carcinogenic potentials as great as organochlorides. Ozonolysis is more expensive than chlorination, and because the ozone cannot be stored, it must be produced on site (by electric discharge in air). Ozone also does not provide a long-term disinfectant action in the distribution system, and so some chlorination remains necessary. Another potential oxidizing agent for water puri®cation is chlorine dioxide, also used in a few localities. This compound is unstable and cannot be stored; it must be prepared on site from sodium chlorite, usually by the reaction of chlorine, NaClO2 ‡ 1=2Cl2 ! ClO2 ‡ Na‡ ‡ Cl

…11-14†

although an alternative preparation method is to treat the chlorite with acid. In both cases, side reactions produce chlorate, a substance whose health effects do not seem to be fully studied. A third, more economical but more complex, method used in some pulp and paper mills involves reduction, in a strong acid solution of sodium chlorate, NaClO3 , with a reducing agent such as SO2 . Because it acts as an oxidizer, chlorine dioxide is reduced to the chlorite ion: ClO2 ‡ e ! ClO2 : !8 ‡ 0954 V

…11-15†

It is not as effective a chlorinating agent as HOCl, and it does not produce CHCl3 or chloramines, but there is some evidence that if organic material is in excess, ClO2 can produce partially oxidized materials such as epoxides, quinones, and chlorinated quinones. It has no residual disinfecting action. Ultraviolet irradiation is still another puri®cation technique that has received limited use (e.g., in Switzerland). It is rapid and independent of pH and temperature, but less effective if suspended matter is present. Passage of water through beds of activated carbon will remove organic contaminants that are not oxidized readily by the chlorine treatment and will also remove chlorinated organic molecules. This process has been used on a limited scale in water treatment plants for many years. It can also be employed by the householder in an attachment to the water tap. Activated carbon is produced by charring a variety of organic materials, followed by partial oxidation. This material has a high surface area and adsorbs most organic molecules effectively. The activity can be regenerated by oxidation of the adsorbed materials by heating in an atmosphere of air and steam. This method is perhaps the most practical means now available for removing chlorinated hydrocarbons, aromatics, and so on, which are among the most dangerous of the organic pollutants likely to be present in a domestic water source.

432

11.5 WATER TREATMENT

11.5.2 Wastewater Treatment Clean water is a vital commodity, and usage is now so extensive that wastewaters must be repuri®ed to avoid destruction of aquatic ecosystems and because, often, the water will be reused. Industrial wastewater may require specialized treatment that depends on the contaminants, while treatment of domestic waste (sewage) involves more general procedures. A great deal of water is used for cooling purposes. Such water, if discharged back to freshwater systems, could lead to so-called thermal pollution by increasing lake and stream temperatures. Impurities are introduced only if additives are present to reduce fouling of heat exchangers (a common practice) or if substances are dissolved from them. Trace metals extracted as corrosion products would be possible examples of the latter case. The chemistry of thermal pollution lies chie¯y in the effects of temperature on physicochemical and biological processes. For example, warm water will reduce the solubility of O2 , thus lowering its capacity to support life and to oxidize impurities. Large amounts of arti®cially warmed water, which will alter the relative volumes of the epilimnion and hypolimnion in a lake, may maintain the density gradient when normal conditions would lead to turnover (Section 9.1.2). Since ®sh and other aquatic organisms often prefer very restricted temperature conditions, the volumes of the habitats available for different species, and therefore the population balance of the water system, may be changed greatly. Dedicated cooling ponds from which the water may be recirculated or cooling towers which transfer the heat to the air, for example by evaporation as the hot water is sprayed through the tower, are alternatives to direct discharge. Use of the discharge water to heat buildings, greenhouses, and the like is attractive if such facilities are nearby. Treatment of domestic wastewater (i.e., sewage) is important, and some steps used in common processes are described brie¯y below. Depending on the ®nal water quality desired, treatment may be at the primary, secondary, or tertiary level. A typical treatment scheme is shown in Figure 11-5. 11.5.2.1 Primary Sewage Treatment

Domestic wastewater normally contains about 0.1 wt % impurities, composed mostly of a variety of organic materials. Many of these can be removed by ®ltration or sedimentation. Large particles (grit, paper, etc.) are removed by coarse mechanical screening followed by settling. Much suspended and ®ne particulate material remains, which is usually removed by sedimentation processes. Floating material such as grease can be skimmed off the top. In welldesigned settling tanks, nearly 90% of the total solids and perhaps 40% of the organic matter can be removed. To remove the smaller particles, however,

433

11. WATER SYSTEMS AND WATER TREATMENT

Raw sewage

Large particles Small/suspended particles Dissolved organics Dissolved inorganics Nutrients Heavy metals

Removes large particles

Screening

Removes small particles

Settling/flocculation

Removes most organics, some nutrients

Sludge Bacterial treatment Sludge To disposal or tertiary treatment

FIGURE 11-5 Typical steps in primary and secondary sewage treatment.

assistance is needed and coagulation may be employed. This process, using aluminum sulfate, ferrous sulfate, or similar compounds, was discussed for drinking water puri®cation in Section 11.5.1. The process is very similar when applied to wastewater. In practice, sewage waters often contain considerable bicarbonate ion that can act as a base; CaCO3 may be part of the precipitate. Lime, Ca…OH†2 , alone will cause CaCO3 to precipitate and has some coagulant action. An added value to using calcium, iron, or aluminum in this process is that much of the phosphorus present can be removed as the insoluble phosphate salts. Up to 95% removal of phosphate is possible. The solid produced in this process, which may contain toxic industrial wastes, grease, bacteria, and other substances, must be disposed of. It is often buried in land®ll, or sometimes dumped at sea, although this mode of disposal is being phased out in many countries. The coarse materials removed in the preliminary steps must be disposed of in a similar way. The treatment processes just described are called primary treatment, and a great deal of sewage receives no further processing. A large amount of dissolved material is left behind. Much of this is organic, but there are also

434

11.5 WATER TREATMENT

nitrate, some phosphate, and metal ions. Secondary treatment removes the organic materials. This is important with respect to the overall quality of the discharged water, since a high organic content will use up the dissolved oxygen in the water, cause reducing conditions and the formation of various undesirable reduction products. Aquatic life also suffers. A practical measure of the reducing impurities in water is the so-called biological oxygen demand (BOD) (Section 7.2.5). 11.5.2.2 Secondary Sewage Treatment

The most widely used method of secondary treatment is a biochemical one, the activated sludge process. Bacterial action decomposes the organic matter in the sewage, producing a bacterial sludge that can be separated by sedimentation for disposal. This sludge is about 1% solids, and amounts to about 700 million gallons per day in the United States. Disposal is a major problem. As of 1993, over one-third (around 2.5 million tons dry weight) was used as fertilizer (often referred to as biosolids, which has a more attractive sound than sewage sludge), around 40% was land®lled, and under 20% incinerated. An even larger fraction of sewage sludge is used as fertilizer in Europe. Use as a fertilizer is attractive: there is signi®cant N, P, and S content; but perhaps more signi®cantly the practice builds up the organic content of soils, which in turn generally supports the natural soil biota and improves soil quality. Most is used in farmland, but other major uses are forest restoration and rejuvenation of mining areas. There are restrictions on the areas where sludge can be used to avoid excessive runoff, and other regulations limit the buildup of toxic materials from repeated applications. It is the possibility of introducing toxic materials that give rise to the greatest objections to this use. There are three categories of concern. 1. "
 . Various harmful organisms remain in the sludge, although they are maintained at acceptable levels and have not been directly implicated in disease. Various treatments are available to reduce these undesirable components to below detectable levels, but they are not used in most facilities. 2. #   $ 
  . Highly stable materials such as dioxins and PCBs (Section 8.7) may be present, especially if the sewage contains industrial wastes. Numerous tests have shown that levels in most sewage sludge are small. 3. %$ 
&  
. These known components of the wastes accumulate in soils in which they are used; take-up by plants can introduce them into the food supply, thus limiting long-term application of biosolids to agricultural land. These limits are indicated in Table 11-5. It is notable that European and U.S. standards are quite different. U.S. standards are based on risk estimates to humans based on various pathways for possible ingestion by humans, while

435

11. WATER SYSTEMS AND WATER TREATMENT

TABLE 11-5 Allowable Limits of Metals in Soils Treated with Sewage Sludge, (mg=kg) Standards

Cd

Cu

Cr

Hg

Ni

Pb

Zn

United States European

20 3

750 140

1500 150

8 1.5

210 75

150 300

1400 300

European standards are based on possible direct ecological effects on the biota of the soils. Alternate sludge processing methods involve further bacterial digestion. Anaerobic digestion of the sludge converts carbon compounds chie¯y to CH4 and CO2 , while nitrate, sulfate, and phosphate are converted at least in part to NH3 , H2 S, and PH3 . About 70% of the gaseous products is methane. This can be burned to heat the reaction tanks, power pumps, and so on, and in fact such degradation of organic wastes to methane is a possible source of energy (Section 16.4). The other gaseous products (except CO2 ) must be trapped or reacted to less noxious forms. Aerobic digestion of the sludge with no additional source of nutrients results in autoxidation as the bacterial cells use up their own cell material. The organic materials are converted to CO2 or carbonates, nitrogen, sulfur, and phosphorus to the oxo anions, and the solution ultimately produced is potentially useful as a liquid fertilizer. This approach to activated sludge disposal is comparatively new. An alternative approach to sewage treatment is the use of lagoons, shallow open ponds in which the water can stand for several days to weeks while the biological activity of bacteria and algae under sunlight destroys most of the organic waste. Sludge must be removed from the lagoon periodically and disposed of as in other treatments. The ®nal water still contains phosphorus and nitrogen nutrients. This approach depends on climate and available land areas.

11.5.2.3 Tertiary Sewage Treatment

Final cleanup of the water ef¯uent from the secondary treatment is called tertiary treatment. Several types of materials must be considered in this respect. It should be kept in mind that while there are many tertiary treatment approaches, they are expensive and not widely used. Even secondary treatment is often not applied in many sewage disposal systems. The speci®c details of waste treatment vary considerably with different sewage handling facilities.

436

11.5 WATER TREATMENT

a. Colloidal Organic Matter

The remains of the activated sludge that do not settle out in the sedimentation tanks are returned to as colloidal organic matter. Different types of ®lter can be used, and it is common at this point to use an Al2 …SO4 †3 coagulation process as described earlier as the key step in aiding the removal of these materials. b. Phosphate

A phosphate concentration of 1 mg=liter is adequate to support extensive algal growth (blooms). Typical raw wastes contain about 25 mg of phosphate per liter. Thus, a large reduction is necessary to ensure that these ef¯uents do not contribute to eutrophication of lakes. Removal of phosphorus by precipitation of an insoluble salt has been mentioned in connection with primary waste treatment. In fact, this precipitation may be done in the primary, secondary, or tertiary step. Lime is commonly used, with hydroxyapatite being the product: 5Ca…OH†2 ‡ 3HPO24 ! Ca5 OH…PO4 †3 ‡ 3H2 O ‡ 6OH

…11-16†

Lime is cheap, and the ef®ciency of phosphate removal is theoretically very high, although colloid formation by the hydroxyapatite, slow precipitation, and other problems often reduce this ef®ciency in practice. Polyphosphates, if present, form soluble calcium complexes (Section 10.5). Other precipitants are MgSO4 (giving MgNH4 PO4 ), FeCl3 (giving FePO4 ), and Al2 …SO4 †3 (giving AlPO4 ). Phosphate precipitation may occur as part of a coagulation process, especially if iron or aluminum salts are used. An alternate process to precipitation is adsorption, using activated alumina (i.e., acidwashed and dried Al2 O3 ). The alumina can be regenerated by washing with NaOH. c. Nitrate

The activated sludge process converts some nitrogen to organic forms that are removed with the sludge; much, however, remains behind. Converting this to nitrate is possible if excess air is used, but this method of operation, more expensive than ef®ciently removing carbon compounds, is usually not used. The nitrogen remaining in the ef¯uents then is largely some form of ammonia: NH3 or NH‡ 4 . This can be stripped from solution by a stream of air if the solution is basic (the pH can be adjusted to be greater than 11 by the addition of lime, which can simultaneously remove phosphate). The chief problem lies in disposing of the ammonia in the air stream. It can be adsorbed by an acidic reagent, but at further cost. If allowed to escape, it is a potential local air pollutant, and eventually enters the runoff water through rain. Alternatively, aerobic bacterial nitri®cation of ammonia to nitrate, followed by denitri®cation by other bacteria in the presence of a reducing carbon compound (e.g., methanol) can be employed:

11. WATER SYSTEMS AND WATER TREATMENT

nitrifying ! NO3 ‡ H‡ ‡ H2 O bacteria denitrifying ! 3N2 ‡ 5CO2 ‡ 13H2 O 6NO3 ‡ 5CH3 OH ‡ 6H‡ bacteria NH3 ‡ 2O2

437

…11-17† …11-18†

Purely chemical processes for nitrogen removal are not available; suitable insoluble salts do not exist for a precipitation process, but reduction to N2 or N2 O (which can be captured) by Fe(II) has been suggested for possible development.   Organic Material

Comparatively little dissolved organic material remains after secondary treatment, but what remains is signi®cant in terms of taste, odor, and toxicity. Chemical oxidation is a possibility, with a variety of oxidants being proposed, including chlorine, hydrogen peroxide, and ozone. Adsorption on activated carbon is effective and perhaps more practical. e. Dissolved Inorganic Ions

Besides nitrate and phosphate ions, a signi®cant quantity of other inorganic substances is present. Although many of these are not harmful, their accumulation eventually renders water unsuitable for reuse. In addition, toxic heavy metal ions may be present, although most of these precipitate under basic conditions. Avariety of methods can be used to remove these substances, although in general the methods are expensive and rarely used in present tertiary wastewater treatments. When high-quality water is scarce, use of one or more of these methods may be practical as it is with brackish or seawater in arid areas, and for some of them the primary application is in desalinization plants to produce drinking water. Of main interest for desalination are distillation, electrodialysis, reverse osmosis, ion exchange, and freezing. Distillation Distillation is an old technique, and quite simple if the waters do not contain volatile impurities such as ammonia. Although expensive, it has been used for many years to supply fresh water from seawater. Fossil fuel has normally served as the heat source, but solar distillation, the use of solar energy to evaporate the water has low cost potential in suitable areas. Electrodialysis This is a newer technique. Water is passed between membranes that are permeable to positive ions on one side of the water stream and to negative ions on the other. An electrical potential is applied across the system so that the ions migrate, the positive ions passing out through the cation-permeable membrane (which prevents anions from ¯owing in), while the negative ions move out in the opposite direction through the

438

11.5 WATER TREATMENT

anion-permeable, cation-impermeable membrane. The result is a stream of deionized water between the membranes, and this stream can then be separated as clean water. This process is critically dependent on the composition of the water; large ions, for example, do not pass through the membranes. It has been applied to tertiary treatment on a pilot-plant scale. Reverse Osmosis Sometimes called hyper®ltration, reverse osmosis is another newer process for water puri®cation which is widely used. If pure water is separated from an aqueous solution by a membrane (e.g., cellulose acetate) that is permeable to water but not to the solute, then the solvent will ¯ow from the pure water side into the solution. If the apparatus is designed appropriately, a hydrostatic pressure that will counteract the tendency of water to ¯ow into the solution side of the membrane can be developed across the membrane. Without this hydrostatic pressure, liquid level in the solution compartment rises, corresponding to the osmotic pressure of the solution. However, if a hydrostatic pressure exceeding the value of the osmotic pressure is applied to the solution, water will ¯ow from the solution to the clean water side of the membrane. This is the principle of reverse osmosis. The process is in use to obtain pure water from seawater in the Middle East, the Caribbean, on ships, and for some other pure water supplies. In practical systems, a very thin supported membrane is used; very small pores permit the water molecules but not the hydrated metal ions to pass. Ion Exchange Frequently used for small-scale water puri®cation, ion exchange is often found in home water softening devices. Ion exchange materials are usually organic resins, but some inorganic materials can also function in this way. The bulk of the resin carries a charge (e.g., a group such asÐOSO3 or a quaternary amine N‡ ), where an ion of opposite charge is held by Coulombic forces to produce electrical neutrality. An ion of a given charge can be replaced by another, and if those present initially are H‡ on the cation exchanger and OH on the anion exchanger, ionic impurities can be removed completely if water is passed through one and then the other. The exchangers are then regenerated by acid and base solutions, respectively. In household water softening, removing the Ca2‡ ions, replacing them with Na‡ ions, is often adequate. Regeneration can then use an NaCl solution. Partial Freezing This is another method that can be used to produce useable water from a saline or contaminated source. Typically, when a dilute aqueous solution freezes, the ®rst material to solidify is the solvent, water. Ice is formed, while the unfrozen solution becomes more concentrated. This ice can be separated and melted as clean water, and the remaining concentrated solution discarded.

11. WATER SYSTEMS AND WATER TREATMENT

439

11.6 ANAEROBIC SYSTEMS The solubility of molecular oxygen in water is suf®cient to support aerobic organisms and oxidizing conditions in much of the natural water systems that we encounter. However, inef®cient mixing often permits bottom waters of lakes and oceans, and especially the waters in the sediments that underlie them, to become depleted in oxygen as biological processes use it up. This has been mentioned in several places (e.g., Section 9.1.2). Marshes and other systems with large amounts of decaying organic matter, soils with high organic contents and poor drainage, coal deposits, and land®ll sites also lead to groundwaters that are anaerobic. Normal respiration produces energy by the conversion of organic carbon compounds, the composition of which can be approximated by the empirical formula …CH2 O† , to CO2 using oxygen as the oxidizing agent: 1 …CH2 O† ‡ O2 ! CO2 ‡ H2 O 

…11-19†

This produces the maximum energy of any respiration process available to organisms; the free energy change involved in this process being about 500 kJ per ``mole'' of CH2 O. However, several alternative oxidizing agents are available to appropriate anaerobic organisms. One of these alternatives is the nitrate ion: 5 …CH2 O† ‡ 4NO3 ‡ 4H‡ ! 5CO2 ‡ 7H2 O ‡ 2N2 

…11-20†

Use of nitrate in this way is a common process in soils, but nitrate is rarely abundant in sediments. In actuality, the microorganisms that carry out this process do so in several steps: nitrate ! nitrite ! nitrogen oxides ! nitrogen. Some organisms utilize only some of these steps, and intermediates such as nitrous oxide may be released. The total free energy change is smaller than if oxygen were used, 480 kJ per ``mole'' of organic material, which means that nitrate-based metabolism is less ef®cient. As part of the decay process, nitrogen contained in the organic matter is converted to ammonia (recall that biological material contains about 16 nitrogen atoms for every 100 carbon atoms; Section 10.5). Under aerobic conditions, bacteria will oxidize the ammonia that is not assimilated, but under anaerobic conditions it too may be released. Reduction of nitrite to ammonia is somewhat more favorable thermodynamically than reduction to nitrogen, but does not seem to be an important step biochemically. Reduction of nitrogen to ammonia is of course an important biochemical process, but apparently not one that is used for energy production. Sulfate is a second substrate available to anaerobic organisms, particularly in marine environments where sulfate is relatively abundant in seawater.

440

11.7 IRRIGATION WATERS

2 …CH2 O† ‡ SO24 ‡ 2H‡ ! 2CO2 ‡ 2H2 O ‡ H2 S 

…11-21†

It is less energy ef®cient than the nitrate process, with a free energy change of only 103 kJ per ``mole.'' The H2 S produced may be released to the atmosphere, but alternatively it may be precipitated as metal sul®des, since many transition metal and heavier metal sul®des are insoluble. For example, iron, which is relatively abundant, is likely to be present under reducing conditions as Fe2‡ and can then generate ferrous sul®de deposits. Under other (aerobic) conditions, oxidation of sul®de or even of the Fe2‡ can be energy sources for other organisms. In some cases, elemental sulfur can be a by-product. Methane-producing organisms are likely to predominate when nitrate and sulfate concentrations are low. The process is 2 …CH2 O† ! CO2 ‡ CH4 

…11-22†

with only 93 kJ of free energy available per ``mole.'' Methane is frequently produced in marshy areas (swamp gas) and in land®lls. Methane can also be used as an energy source for some bacteria. A similar process can generate hydrogen 1 …CH2 O† ‡ H2 O ! CO2 ‡ 2H2 

…11-23†

with an energy release of about 26.8 kJ.

11.7 IRRIGATION WATERS Much agriculture depends on irrigation. Many of the most fertile soils occur in arid regions. Both surface water and groundwater sources are heavily used. Irrigation, however, is not simply adding enough water to the soil to maintain plant growth; it introduces some serious problems both for the water being used and for the soil itself. These problems relate to the mineral content of the water, which increases through the irrigation process. Inevitably, some water used for irrigation evaporates. The salt content, made up in part from the initial mineral content of the water, but increased by the salt leached from the soil as the water ¯ows through the irrigation system, may reach a level at which further evaporation leads to deposition of additional salts in the soil rather than their removal. An essential feature of long-term irrigation is the need to use enough water to dissolve and carry away excess salts. In some areas, drainage systems are placed below the root level to facilitate this; an example is the San Joaquin Valley in California. Irrigation water quality depends on at least four factors.

11. WATER SYSTEMS AND WATER TREATMENT

441

1. '
( the total salt content of the water. With a high soluble salt content, the soil may become unsuited to plants with low salt tolerance, and the returned irrigation water may be un®t for further use. Salt deposits from successive irrigations may carry deposited salt to lower depths, where it will accumulate in the root zone if adequate leaching does not take place. 2. '     
&   
  

      (called the sodium absorption ratio, SAR). Because of ion exchange reactions with clay minerals in the soil, a high sodium ion content relative to the others can cause breakdown of the soil particles, leading to impermeability to water (waterlogging) and to hardening of the dry soil, even if the total salt concentration is low (Sections 9.7 and 2.3.1). 3. 
( the carbonate and bicarbonate content of the water (Section 9.2.2). This property in¯uences soil pH, but also may result in precipitation of poorly soluble calcium and magnesium carbonates as the water evaporates, leading to an increased SAR for the remaining water. 4. %$   , Some compounds that can be damaging to particular cropsÐfor example, borates in parts of the western United StatesÐmay be present in the source irrigation water. These substances can accumulate in the soil over time, even if the initial levels are not harmful. If enough excess water is used so that salts, carbonates, or toxic materials do not accumulate through evaporation, this excess mineral-laden water becomes runoff, entering either surface water systems or aquifers and perhaps degrading their qualities also. Buildup of toxic elements to hazardous levels can occur. Examples in the United States are boron and selenium (Sections 10.6.8 and 10.6.12), both of which have exceeded acceptable levels in some California irrigation waters. Selenium-rich water from irrigation uses in the San Joaquin Valley draining into the Kesterson Wildlife Refuge in California had serious effects on the aquatic life and wildfowl (it is teratogenic) until the input was stopped.

Additional Reading Baker, L. A., ed., !& 
    )
 
  &, ACS Advances in Chemistry Series 237. American Chemical Society, Washington, DC, 1994. Drever, J. L., %      *
 
 
 . Prentice-Hall, Englewood Cliffs, NJ, 1982. Forster, B. A., %  
  
 . Iowa State University Press, Ames, 1993. Howells, G.,  

   
 , 2nd ed. Ellis Horwood, New York, 1995. Laws, E. A., +
 " ,    % $, 2nd ed. Wiley, New York, 1993. Libes, S. M.,    
    . Wiley, New York, 1992. Sopper, W. E.,  
 '  #  )
 

. Lewis Publishers, Boca Raton, FL, 1993.

442

EXERCISES

EXERCISES 11.1. Describe the changes in pH as typical river water evaporates. What solid products would you expect to deposit? 11.2. What are the ®ve most abundant inorganic materials in seawater? How do these compare with elemental abundance in the environment as a whole? 11.3. Give equations for the reactions of silica in water; of alumina in water. Do these reactions occur to a signi®cant extent in the environment? 11.4. Write some model equations to illustrate how the ocean pH might be determined by reactions involving alumina and silica. 11.5. What are the usual components of acid rain? What are the sources of these acids? What is the relative importance of the different sources? 11.6. Describe the usual geographic patterns of pH of precipitation in the United States and in Europe. Explain the reasons for these patterns. 11.7. We have mentioned acid precipitation in North America and Europe. Is it a problem in other parts of the world? Where else would you anticipate problems from acid precipitation? Explain why. 11.8. List the steps that are usually employed in the treatment of drinking water. 11.9. Use an equation to explain why the disinfectant power of chlorine is pH dependent. 11.10. What are the available practical methods for disinfecting drinking water? Give advantages and disadvantages of each. 11.11. Give equations showing the mechanism of formation of chloroform from acetophenone, C6 H5 C…O†CH3 , as a by-product of water chlorination. 11.12. Describe the chemistry involved in the process of ¯occulation in water treatment. Include equations. 11.13. Describe the processes of primary, secondary, and tertiary sewage treatment. 11.14. Indicate some practical methods for disposing of the sludge from sewage treatment. Compare the advantages and disadvantages of each. 11.15. Give the equations of the reactions that take place in anaerobic metabolic processes. Under what environmental conditions is each expected to be most important? 11.16. Compare the energy available from oxidation of one gram of organic material with O2 , NO3 and SO24 as oxidizing agents. 11.17. Explain how irrigation can lead to deterioration of the agricultural quality of soils.

12 THE EARTH'S CRUST

12.1 ROCKS AND MINERALS Current theories consider the earth to have formed from condensation of dust and gas in space. Gravitational and radiochemical heating melted the aggregated solids, and as the planet cooled, partial solidi®cation and separation of materials took place. The present structure of the earth consists of a largely molten core composed chie¯y of iron and nickel, surrounded by lighter rocks. The outer few miles, the crust, is the only portion of the earth that is accessible, and is the source of most of the substances used in a technological society. The crust has undergone a complex evolution as processes such as weathering and erosion have broken up the original rocks, and sedimentation and crystallization have produced new ones. High pressures and temperatures and volcanic activity have produced other changes. Indeed, these processes continue. These reactions, which fall into the realm of geology and geochemistry, are too extensive to be dealt with in detail here. We will discuss some of the aspects that most strongly impinge on human activity, in particular, those relating to some of the substances that we use extensively. 443

444

12.1 ROCKS AND MINERALS

Many terms describing rocks and minerals are encountered in any discussion of the earth's crust and the processes that take place in it. The terms may describe a speci®c mineral, categorized by a speci®c structure and general composition [e.g., beryl, Be2 Al2 …SiO3 †6 ] a class of related minerals (e. g., feldspars), or a conglomerate with particular properties (e.g., granite). Table 12-1 gives some of the most common of these terms; it is far from complete.

TABLE 12-1 Some Common Mineralogical Terms Amphibole

A class of silicate minerals, containing chie¯y Ca, Mg, and Fe, but also a wide variety of other cations, found in many igneous and metamorphic rocks. The approximate formula is MSiO3 , but the actual Si=O ratio is 4:11. Amphibole also refers to a speci®c mineral of the group, also called hornblende, NaCa2 …Mg, Fe, Al†5 …Si, Al†8 O22 …OH†2 . (Elements in parentheses mean any combination totaling the subscript number.) Many asbestos materials are amphiboles.

Anorthite

A common feldspar, CaAl2 Si2 O8 .

Apatite

A phosphate mineral, Ca5 …OH, F, Cl†…PO4 †3 .

Aragonite

One crystalline form of CaCO3 .

Asbestos

A term used to describe a ®brous form of some aluminosilicates, especially amphiboles but also a ®brous serpentine, chrysotile. Discussed in Section 12.4.5.

Basalt

A type of igneous rock formed on slow cooling; containing iron oxides, feldspar, and other species. The most common volcanic rock, underlies much of the ocean basins.

Bauxite

The primary ore used as a source of aluminum. It is a mixture of the minerals Al…OH†3 (gibbsite) and two forms of AlO(OH) (diaspore and boehmite).

Calcite

One crystalline form of CaCO3 , the most stable under ambient conditions.

Clay

Aluminosilicates with layer structures; weathering products of other aluminosilicate rocks and usually existing as small platelike particles. Also used to refer to any mineral of particle size under 2 mm.

Crocidolite

The most common amphibole asbestos, Na2 Fe4 Al2 Si8 O22 …OH†2 . It is the ®brous (asbestiform) version of the mineral riebeckite.

Cryolite

The mineral Na3 AlF6 .

Chrysotile

A serpentine (see below) asbestos, Mg3 Si2 O5 …OH†4 .

Dolomite

The mineral CaMg…CO3 †2 . (continues)

445

12. THE EARTH'S CRUST

TABLE 12.1 (continued ) Feldspar

A mineral group that is the most abundant in the earth's crust. Feldspars are the major constituents of igneous rocks and also important in most sedimentary and metamorphic rocks. The general composition is KAlSi3 O8 , but Na often substitutes for K, or another Al substitutes for a Si with the charge balance maintained by substitution of Ca or Ba for some or all of the alkali metal.

Granite

A common igneous rock formed on slow cooling; it is mostly quartz and feldspar.

Hematite

The mineral Fe2 O3 .

Igneous rocks

Rock formed on cooling of magma, the molten rock released from below the earth's surface by volcanic action. It consists of tightly interlocked crystallites of a variety of speci®c minerals.

Kaolinite

A common clay mineral, Al4 Si4 O10 …OH†8 .

Limestone

A sedimentary rock, usually deposited through biological processes, and mostly calcium carbonate.

Magnetite

Fe3 O4 ; a combination of Fe(II) and Fe(III). It is an example of a spinel (a class of minerals based on the composition M…II†M0 …III†2 O4 .

Marble

Metamorphosed limestone, CaCO3 .

Metamorphic rocks

A rock that has undergone change under high temperature and pressure, aided by chemical action (e.g., of water).

Mica

A group of aluminosilicate minerals with a sheetlike structure. Micas contain potassium and hydrogen, and often other elements. An example is muscovite.

Microcline

A common feldspar, KSi3 O8 (the same formula as orthoclase but a different crystal structure).

Montmorillonite

A common smectic clay, …Ca, Mg†Al2 Si5 O14
nH2 O. (Smectic refers to the property of swelling when wet.)

Muscovite

The most common mica mineral, KAl3 …OH†2 Si3 O10

Olivine

A group of abundant minerals in igneous rocks, with compositions running continuously from Mg2 SiO4 (forsterite) to Fe2 SiO4 (fayalite) and containing also Ca, Mg, and Mn as common bivalent cations.

Orthoclase

A common feldspar, KSi3 O8 (the same formula as microcline, but a different crystal structure).

Plagioclase

Feldspars with Na or Ca as the primary cations (e.g., anorthite, CaAl2 Si2 O8 ).

Pyrite

The mineral FeS2 (fool's gold), which contains the S22 ion. The term pyrite is sometimes used for related metal disul®des.

Pyroxene

A group of silicate minerals found in igneous and some metamorphic rocks. Their compositions are MSiO3 . An example is diopside, CaMgSi2 O6 .

Quartz

Crystalline SiO2 . Rocks composed mostly of quartz are called quartzite. (continues)

446

12.1 ROCKS AND MINERALS

TABLE 12.1 (continued ) Sandstone

A sedimentary rock composed of sand, mostly quartz but sometimes particles of feldspar or other minerals, cemented together with calcium carbonate, silica, an iron oxide, or a claylike mineral. The properties depend very much on the cementing material.

Sedimentary rocks

Rock formed from sediment deposits of material derived from the disintegration of another rock.

Serpentine

A group of layered-structure magnesium silicate minerals derived from the kaolinite type of aluminosilicates by replacement of Al by Mg. A ®brous form is the asbestos called chrysotile. Another example is talc, Mg3 Si4 O10 …OH†2 .

Shale

A sedimentary rock formed from mud, silt, or clay.

Slate

Rock formed by the metamorphosis of shale.

Zeolite

Aluminosilicate minerals with molecular-sized pores that can adsorb small molecules. Many synthetic zeolites have been made because of their adsorption and catalytic powers. Also used as ``builders'' in detergents in place of phosphates.

Table 12-2 gives the relative abundances of the most common elements in the earth's crust. As can be seen, by far the largest part of the crust is made up of silicon and oxygen, which form the basis of the abundant silicate minerals. TABLE 12-2 Relative Abundance of Some Elements in the Earth's Crust Element

Abundance (at. %)

Oxygen

63

Silicon Aluminum Iron Calcium Sodium Potassium Magnesium Titanium Hydrogen Manganese Phosphorus Cu, Cr, Ni, Pb, Zn Mn, Sn, U, W Ag, Hg Au, Pt

21 6.5 1.9 1.9 2.6 1.4 1.8

Abundance (wt %) 47 28 8 5 3.6 2.8 2.6 2.1 0.44 0.14 0.1 0.1 102 103 each  10 4 each  10 6 each  10 7 each

12. THE EARTH'S CRUST

447

The fundamental structure of all silicates consists of four oxygen atoms tetrahedrally arranged around a central silicon atom. In terms of oxidation numbers, these are considered to be Si…4† and O(±2) (oxidation states Si(IV) and O(±II)), but the SiÐO bonding is covalent. However, an isolated SiO4 tetrahedron would carry a charge of ±4. Minerals based on the simple SiO4 4 ion in association with cations (salts of silicic acid, Section 11.2) are unusual, and more typically the natural silicates are based on rings, sheets, and chains of linked tetrahedra in which the Si atoms share oxygens. The O:Si ratio is less than 4. Some typical structures are given in Figure 12-1. In aluminosilicates, aluminum, the third most abundant element in the earth's crust, is also present, surrounded tetrahedrally or octahedrally by oxygen atoms. In all these structures, negative charges on the silicate framework require the presence of cations for electrical neutrality. Within limits, the nature of the cationic species is of secondary importance. Particular structures are favored by particular cations to maximize crystal packing energies, Coulombic attractions, and other interactions leading to stabilization of the solid, but small amounts of many cations can be present in a given structure without in¯uencing it in any major way. In particular, ions of similar size and charge may replace one another with little change in mineral structure (isomorphous substitution). If the similarity is great enough, complete replacement of one component by another can take place without signi®cant structure change. As the similarity becomes less, then less replacement can take place in a given mineral before the structure changes. (Such behavior holds for many solid materials besides silicate minerals.) From Table 12-2 it is seen that many of the elements essential for modern technology are present in very small amounts in the earth's crust compared with the dozen most abundant elements. The total amounts of these less abundant elements in the earth's crust are vast, however, and they are widely distributed. Most common rocks contain a few parts per million of many elements distributed randomly by isomorphous substitution of abundant elements (e.g., Pb replaces some K, and Zn replaces some Mg in most common rocks). For this reason, it has been suggested that humanity will never really run out of mineral resources, and as high-concentration ores are exhausted, new technology can be developed to tap the sources in the common rocks. However, the volume of material to be mined and processed, the energy requirements, and the waste disposal problems clearly set economic and environmental restrictions on the minimum concentrations that can be employed for large-scale use of any substance. Generally, society uses atypical, highconcentration sources for most of its mineral needs; little if any technological development would have been possible in the past if all elements were uniformly distributed in the earth's crust.

448

12.1 ROCKS AND MINERALS

(a)

(c)

(b)

(e)

(d)

(f)

(g) FIGURE 12-1 Examples of silicate structural units: (a) the SiO4 tetrahedron; (b) a schematic view of a SiO4 tetrahedron, where each apex represents an oxygen; (c) linked tetrahedra, the Si2 O6 7 ion; (d) a chain structure; (e) a cyclic silicate structure; (f) a double chain; and (g) a twodimensional layered structure.

Imminent shortages of many metals were predicted during the third quarter of the twentieth century. These shortages have not materialized, partly because of improved methods of exploration, partly because of improved mining technology, and partly because of decreased demand and increased recycling. Current reserves of metal ores are adequate for many years.1 1

C. A. Hodges, Science, 268, 1305 (1995).

12. THE EARTH'S CRUST

449

12.2 RECOVERY OF METALS FROM THEIR ORES 12.2.1 Sources Minerals used as sources from which desired elements can be isolated are called ores. The ores of many elements are made up from particular compounds of the element in question, although these may be mixed with much inert rock. High-grade ores typically consist of veins of the compound; in lowgrade ores the particles may be widely distributed in the rock. Mining may involve tunneling along the ore veins or open pit quarrying of large volumes of rock. The latter is particularly necessary when low-grade ores are used, as is becoming more common, and as modern earthmoving equipment makes this technique economical. Placer mining which involves recovery from riverbed gravels, is important in gold mining. Mining has traditionally caused considerable environmental impact owing to the obvious damage to the land from the excavation itself, the waste rock deposits, and the disruption of rivers and streams. Less obvious but perhaps more critical are the effects from acid mine wastes (see Section 10.6.3) and solubilization of heavy metals. At least 50 abandoned mine sites in the United States have been designated as hazardous under the Superfund program.2 Ore bodies in nature were formed in a number of ways: for example, by selective crystallization as the molten material (magma) cooled to form rocks, and by hydrothermal processes, which have been important for many widely used metals. In a hydrothermal process, water or brine at high temperature and pressure dissolves metal ions from the bulk rock and redeposits them in concentrated form elsewhere. The extraction process is analogous to a weathering reaction. Exploitable deposits typically formed where the liquid ¯owed through a restricted channel in which a precipitation reaction could take place. Formation of very insoluble sul®des and arsenides has provided many ore bodies. Oxides and carbonates are among the other most common ore minerals. Ongoing deposition at ocean hydrothermal vents may represent a present-day example of ore body formation. Hydrothermal circulation involves seawater penetrating into the ocean crust, where it is heated geothermally. Magnesium and sulfate are removed through interactions with the rocks, while at the same time components from the rocks are leached into the water. Conditions are normally reducing, resulting in formation of H2 S and sul®des, and metal ions such as Fe in reduced states. Under the high temperature and pressure of the crust, many of these are soluble. As the hot water rises, cooling allows deposition of secondary minerals such as metal sul®des and quartz as their solubility decreases. If by the time the water has reached the crustal surface it is still hot 2

The Superfund program is a federal plan for funding the costs of cleanup of seriously polluted waste disposal and other sites.

450

12.2 RECOVERY OF METALS FROM THEIR ORES

enough to have retained a high mineral content, rapid mixing with the cold seawater results in formation of an immediate precipitate that contains materials such as FeS, ZnS, CuFeS2 , CaSO4 , and BaSO4 (the minerals pyrrhotite, sphalerite, chalcopyrite, anhydrate, and barite, respectively). Since many of theses are black, the cloud of precipitating minerals around the release point gets the name black smoker; generally this cloud is accompanied by buildup of a ``chimney'' of precipitated minerals. The process is shown schematically in Figure 12-2. These systems are important not only for their inorganic chemistry, but also for the unusual biological activity that they support, based on the use of reduced mineral compounds as energy sources by certain bacteria that are capable of thriving under high-temperature conditions and of utilizing the energy released in biological oxidation of the reduced species to support their metabolism. These life-forms make up a class of organisms that are not dependent on solar radiation for their ultimate energy source. Some speci®c ores and treatments used for individual metals are listed in Table 12-3.

2⬚C

0.1 cm/s

Oxyanions, (HPO42–, HVO42–,CrO42–, HAsO42–), REE, Trace metals

3He,

Mn2+, H4SiO4, FeOOH, MnO2, T, CH4, Fe2+, FexSy, 222Rn, H2, H2S 2.05⬚C Black smoker

Basalt

WARM (diffuse) 2–60⬚C

r ate

w Sea

Sub seafloor microbial biosphere

Basalt

HOT (focused) 350⬚C

Seaw

Spreading

Fe-Mn crusts

H+, Cl–, Mn2+, H4SiO4, 3He, H S, CH , CO , H , 2 4 2 2 Ca2+, K+, Li+, Cu2+, Zn2+, Pb2+

e

r

–SO42–

Metalliferous sediments

Axis

ater

–Mg2+

Precipitation chimney

E v olv

e

ea ds

w

at

HT Reaction zone 400⬚C

Fe2+,

MAGMA 1200⬚C

FIGURE 12-2 Processes involved in hydrothermal vent geochemistry. REE, rare earth elements. From U. S. Department of Commerce National Oceanic and Atmospheric Administration: www.pmel.noaa.gov=vents=chemistry=information.html

451

12. THE EARTH'S CRUST

TABLE 12-3 Processes Used to Recover Some Metals from Their Ores Metal

Chief ores

Common treatment processes

Comments

Aluminum

Bauxite, a combination of alumina clays

Puri®cation with aqueous NaOH to give Al2 O3 followed by electrolysis in molten cryolite, Na3 AlF6 .

Waste sludge of silicates and Fe2 O3 . Requires abundant electrical energy. Release of ¯uoride compounds.

Cadmium

Zinc ores

Volatilized from crude Zn and collected in ¯ue dust, or precipitated from Zn solutions. Separated from Zn by distillation or electrolysis.

A by-product of Zn production.

Chromium

Chromite, Fe…CrO2 †2

Reduction of ore with C produces ferrochrome alloy. This is dissolved in H2 SO4 , and Cr is then obtained by electrolysis. Alternatively, Cr2 O3 can be formed and reduced with Al, C, or Si.

Cobalt

Smaltite (CoAS2 ), cobaltite (CoAsS), and other arsenides, sul®des, or oxides

Ore roasted to oxide (see Section 12.2.2.2). May be reduced to a mixture of metals, dissolved in H2 SO4 , other metals separated, and Co obtained by electrolysis or by precipitation as Co…OH†3 with NaOCl; heating to oxide followed by reduction by C or H2 gives Co.

Usually a by-product of the production of other metals (e.g., Cu, Pb, Ni).

Copper

Copper pyrite (CuFeS), cuprite (CuO), malachite [Cu2 …OH†2 CO3 ], and various arsenide, oxide, and carbonate ores

Ore concentrate is heated in air to remove some S, As, and Sb, then fused with silica; copper and iron sul®des and oxides separate (copper matte) from an iron silicate slag. The matte is oxidized in the presence of silica:

Much SO2 released in the smelting process, along with As and Sb oxides; both gas and dust discharges involved. Also aqueous waste from the re®ning process. Anodic sludge is a source of Ag and Au. It also contains Se, Te, and heavy metals.

2FeS  3O2  SiO2 ! iron silicate slag 3Cu2 S ‡ 3O2 ! 6Cu ‡ 3SO2

Crude Cu anode re®ned electrolytically; crude Cu anode dissolves in H2 SO4 CuSO4 electrolyte and deposits as pure Cu cathode. (continues)

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12.2 RECOVERY OF METALS FROM THEIR ORES

TABLE 12.3 (continued ) Metal Gold

Chief ores Free metal, usually ®nely divided in rock.

Common treatment processes Finely divided ore treated with aqueous cyanide solution and air; 4Au  16NaCN  3O2 ! 4NaAu…CN†4 ‡12NaOH; then 2‰Au…CN†4 Š ‡ 3Zn ‡ 4CN ! 2Au ‡ 3‰Zn…CN†4 Š2 A lower technology process dissolves the Au in metallic mercury with recovery by distillation of the Hg.

Comments Cyanide wastes can cause serious water pollution problems. Use of Hg releases metallic mercury to the environment; in primitive mining operations, the distilled Hg may not be condensed.

Iron

Magnetite (Fe3 O3 ), hematite (Fe2 O3 ), limonite (2Fe2 O3
3H2 O), siderite (FeCO3 ).

Oxides reduced in a blast furnace with coke and limestone; carbonates are ®rst roasted to oxide. Puri®cation and steel making involve oxidation of C, Si, S, and P with O2 and removal as CO2 and as a slag formed with the limestone ¯ux (see Section 12.2.2.2).

Large volumes of CO2 gas produced, and Fe2 O3 and Fe3 O4 as dusts.

Lead

Galena (PbS), cerussite (PbCO3 ), anglesite (PbSO4 , and others

Sul®de ores are oxidized:

Much SO2 is produced; As and Sb are often present and are released as oxides.

Manganese

Oxides (e.g., pyrolusite, MnO2 ) and some carbonates and silicates.

Ferromanganese ( 80% Mn) produced in a process similar to that used for Fe; pure metal is produced electrolytically from MnO2 dissolved in sulfate solution.

Mercury

Cinnabar (HgS).

Roasted with air and the mercury vapors condensed:

3PbS ‡ 3O2 ! 3Pb ‡ 3SO2

HgS ‡ O2 ! Hg ‡ SO2

Molybdenum

Molybdenite (MoS2 ).

Alternatively, roasted with Fe or CaO; metal sul®des and=or sulfates produced instead of SO2 Concentrated and roasted to MoO3 , then reduced with H2

SO2 produced.

(continues)

453

12. THE EARTH'S CRUST

TABLE 12.3 (continued ) Metal

Chief ores

Common treatment processes

Nickel

Pentlandite [(Ni,Fe)S], oxides, silicates, and arsenides.

Usually occurs with Fe and Cu. Fractionated by ¯otation, melted to a matte as with Cu and converted to NiO. Reduced with C or water gas, and puri®ed by conversion to Ni…CO†4 , volatilized, and thermally decomposed back to the metal; alternatively, electrolysis.

Silver

Argentite (AgS), cerargyrite (AgCl) pyrargyrite (AgSSb), and other sul®de and antimonide ores.

By-product of Cu, Pb, and Zn ores; obtained during re®ning of the base metal. With Cu, the Ag is obtained from the anode slime and is recovered by roasting, leaching with H2 SO4 , and smelting to remove Se, Te, and other impurities.

Tin

Cassiterite (SnO2 ). Stannite (Cu2 FeSn S4 )

Roasted as necessary to remove S as SO2 and As as As2 O3 , and the tin oxide reduced by C.

Titanium

Ilmenite (FeTiO3 ), rutile (TiO2 ).

The oxide is converted to the tetrachloride, which is reduced by magnesium:

Comments Same as Cu.

2TiO2  3C  4Cl2 ! 2TiCl4 ‡2CO ‡ CO2 ; then TiCl4 ‡ 2Mg ! Ti ‡ 2MgCl2 Tungsten

Scheelite (CaWO4 ), wolframite […FeMn†WO4 ].

The ore is roasted with Na2 CO3 and NaNO3 , leached, and the tungstate precipitated with HCl as tungstic acid. This is calcined to WO3 and reduced to metal with H2 .

Zinc

Sphalerite (ZnS), carbonates.

The ore is roasted to ZnO, which is reduced with CO; the Zn vaporizes and is collected by condensation. It may be puri®ed by distillation.

SO2 is evolved in the roasting. Cd is a common associate; it has a higher volatility.

For all metals, it would seem economically preferable to recycle used metal, since this would eliminate the concentration and reduction steps necessary for virgin materials. Unfortunately, collection and sorting are also energy-intensive

454

12.2 RECOVERY OF METALS FROM THEIR ORES

processes. Moreover, under cheap energy conditions, many processes have been developed without recycling as a major objective. No reprocessing can tolerate the presence of components (metallic or otherwise) that the re®ning steps are not designed to remove and that can produce deleterious properties in the ®nal product. Thus, sorting and separation may have to be extensive. However, as waste disposal becomes more dif®cult, recycling must be increased for economic reasons as well as for conservation ones. Recycling is discussed further in Chapter 16. The recovery of a metal from its ore, smelting, has historically been another major source of pollution. Sulfur oxides from sul®de ores have been a major emission, but dusts containing toxic elements such as selenium and heavy metals also have been of concern. Modern smelters can eliminate most of these problems. The details of the metal recovery process depend on the metal and often on the exact composition of the ore used. However, some steps employed are common enough to be discussed in general terms.

12.2.2 Ore Treatment 12.2.2.1 Concentration (Bene®ciation)

Unless the ore is very rich, it is typically concentrated; that is, much of the worthless rock is separated physically from the desired phase. In all such processes the ore is ®rst ®nely ground. In the common ¯otation method, the ore particles are suspended in water in the presence of ¯otation agents. The molecules of the ¯otation agent may attach themselves preferentially to the desired particles rather than to the worthless rock, rendering these particles hydrophobic, hence not wet table by water. They are then carried to the surface in foam when air bubbles are streamed through the water and can be skimmed off. Typical ¯otation agents used for CuS ores are alkali xanthate salts, S R O C

(R = alkyl group)

S

which are surfactants analogous to detergents (Chapter 7), with an af®nity for the metal sul®de particle. Other concentration methods involve, for example, density differences and magnetic separations. In an alternate approach, the metals may be extracted in solution from the crushed rock by chemical or bacterial action (Section 12.2.1). A common chemical treatment uses cyanide, usually as NaCN, and is discussed in connection with gold mining in Section 12.2.6, although it is also used in silver mining and in the recovery of some common metals. Both the bacterial and chemical processes produce large pools of solution that are often acidic, with a high

12. THE EARTH'S CRUST

455

metal content. An example of the considerable potential for environmental damage if the containment fails is the release of several million gallons of acidic, metal-rich sludge and water into the Guadiamar River and surrounding areas in Spain in 1998 after a holding dam at a mining site failed. Other releases are referred to in Section 12.2.6. Even exposure of waste rock to air, water, and bacterial action may allow the release of residual heavy metals in soluble forms, which can enter water systems. 12.2.2.2 Roasting

Sul®de and arsenide ores, and some others, are heated with air at high temperature to convert them to oxides. This process may also involve the use of limestone or some other ¯ux3 that will permit removal of silicate materials, which react with the ¯ux to form a molten slag. The slag can then be separated from the desired material that is insoluble in it. With sul®de ores, SO2 is a major gaseous product and must be trapped to avoid air pollution problems, as discussed in Section 10.4. Arsenic oxide, As2 O3 , is another common product that volatilizes from the furnace but can be condensed to a solid at room temperature. Particulate materials are also given off to the atmosphere unless trapped or precipitated. Possible water pollution problems come from water used to scrub exhaust gases and to cool slag, and from aqueous treatment of the oxides in some processes. 12.2.2.3 Reduction

The oxides produced as just described, or oxide ores, must be reduced to the elemental metal. Carbon, as metallurgical coke made from low sulfur coal, is a common reducing agent. This reduction is carried out at high temperature, such as in blast furnaces, and offers the same waste control problems already mentioned. Large volumes of very hot gases are involved. Other reduction procedures are in use for some elements; electrochemical reduction of alumina is an obvious example. Some examples of these processes are described shortly. 12.2.2.4 Re®ning or Puri®cation

Often the metal obtained initially is too impure for industrial uses. Impurities may be other metals or nonmetals such as S or P that can have very deleterious effects on the physical properties of the metal. Re®ning techniques may involve remelting of the metal and selective oxidation of the undesirable impurities, or electrolytic puri®cation in which the impure metal is dissolved chemically or 3

A ¯ux is a material that will combine with some of the reaction products to form an easily melted phase, called a slag.

456

12.2 RECOVERY OF METALS FROM THEIR ORES

electrolytically and plated out in pure form on the cathode of an electrochemical cell. Many ores are used as sources for several elements, so that actual ¯ow schemes for metal recovery may be elaborate. In addition, unwanted elements are usually present, and if these include toxic materials (Chapter 10), considerable care must be taken in waste disposal practices. Many metal smelters and re®neries in the past were noted for their air and water pollution.

12.2.3 Bacterial Mining The discussion of acid mine drainage (Section 10.6.3) alluded to the ability of bacteria to use metal sul®des in their metabolism, and this capacity is the basis of applications of bacterial attack on sul®de ores to liberate the metals in a useful form. Such processes, which can be referred to as microbial mining,4 permit recovery of metals from low-grade sources in an economical way. The most common bacterium involved in these processes is Thiobacillus ferrooxidans, which occurs naturally in some sul®de minerals. By oxidizing the sul®de to obtain energy, the microbe produces sulfate and releases the metal as soluble metal sulfate. In the copper recovery process, low-grade ore is simply treated with sulfuric acid to encourage growth of the acidophile bacteria, and the dilute copper sulfate solution leaching from the ore pile is collected in a catch basin. The copper can then be recovered by electrolysis and the acidic solution recycled. The normal high-temperature oxidation, with release of gaseous SO2 and related air pollution or scrubbing problems, are thus avoided. About 25% of current worldwide copper production is based on this process. Commercial gold mining is also beginning to apply this method to release gold from low grade sul®de mineral deposits so that it can be recovered by cyanide extraction. Even nonmetallic resources are being extracted in this way. A different bacterium is capable of solubilizing phosphate from its ores, thereby avoiding the usual sulfuric acid treatment and the production of large amounts of calcium sulfate by-product. Bacteria commonly used in these processes have several limitations, such as sensitivity to poisoning by heavy metals and inability to function at the elevated temperatures that the biooxidation process can sometimes produce. Some strains are protected from heavy metals by special enzymes, however, and proper selection or genetic engineering of new strains may avoid this problem. Use of thermophilic bacteria from hot springs and deep sea vents shows promise of permitting higher temperature operation.

4

A. S. Moffat, Science, 264, 778 (1994).

457

12. THE EARTH'S CRUST

12.2.4 Iron Because iron is re®ned in greater amounts than any other metal, some processes used to obtain the metal will be discussed. The oxide (carbonate ores are ®rst heated to decompose them to the oxide) is reduced directly in a blast furnace with coke, limestone being used as a ¯ux. The solids pass down the furnace against a current of heated air that reacts with part of the coke to heat the ore. The liquid iron produced runs to the bottom of the furnace, while the liquid calcium silicate phase (slag) ¯oats above it. The reactions that take place can be summarized as follows: 3Fe2 O3  CO ! 2Fe3 O4 ‡ CO2

…12-1†

Fe3 O4 ‡ 4CO ! 3Fe ‡ 4CO2

…12-2†

Fe2 O3 ‡ CO ! 2FeO ‡ CO2

…12-3†

FeO ‡ C ! Fe ‡ CO

…12-4†

The limestone decomposes and reacts with the silica: CaCO3 ! CaO ‡ CO2

…12-5†

CaO ‡ SiO2 ! CaSiO3 …slag†

…12-6†

Reaction (12-6) is oversimpli®ed; the slag is not pure calcium silicate. The limestone also removes sul®des that may be present through the reaction FeS ‡ CaO ‡ C ! CaS ‡ Fe ‡ CO

…12-7†

but excess sul®de is undesirable; hence the requirement that the coke be made from low-sulfur coal. Some silica is reduced to Si, and phosphate to P. The product of the blast furnace, pig iron, ordinarily contains about 2% P, 2.5% Si, more than 0.1% S, 4% C, and 2.5% Mn by weight. The latter element is present in the iron ore and goes through reactions similar to those of Fe. Puri®cation to give a steel of improved physical properties is necessary for most purposes. In particular, P, S, Si, and C must be removed or reduced in amount. In the now obsolete open hearth method, the pig iron with perhaps 40% scrap iron, limestone ¯ux, and some Fe2 O3 and Fe3 O4 is melted in a furnace heated by gas and air. The P, C, Si, and S are oxidized, and the silicate and phosphate are removed as a slag by reaction with basic CaO. Modern procedures use the basic oxygen process, in which the oxidation is carried out by a stream of oxygen gas. The process requires much less time (the order of half an hour compared with 12 h) and less energy than the open hearth process, but it uses less scrap than the latter and has had some depressive effects on recycling of scrap iron and steels. Special steels, especially those requiring oxidizable components, are made in an electric furnace. This is expensive in terms of energy, but provided the

458

12.2 RECOVERY OF METALS FROM THEIR ORES

overall composition is suitable for the steel being produced, a high proportion of scrap can be used. Particulate matter in the form of iron oxides are the main emissions from the above processes. Although a great deal of carbon monoxide is involved [reactions (12-1)±(12-4)], most of it is recycled. Much water is used for cooling and scrubbing, but one of the most signi®cant processes related to water pollution involves removal of oxide scale from the ®nished steel in a process called pickling. This is achieved in a H2 SO4 or HCl bath: FeO  2H ! Fe2‡ ‡ H2 O

…12-8†

The waste liquors are highly acidic and contain ferrous salts; discharge to a water system is reminiscent of acid mine drainage (Section 10.6.3). Injection into deep wells is one means of disposal, although this could be dangerous with respect to groundwater contamination.

12.2.5 Aluminum Aluminum is also smelted extensively, and the isolation of this metal illustrates the chemistry of an active metal for which chemical reduction is not economically favorable because of the need to use powerful, and consequently expensive, reducing agents. The aluminum ore used virtually exclusively is bauxite, essentially an alumina clay, Al2 O3
2H2 O, along with other minerals, often including iron oxide. Alumina, Al2 O3 , can be recovered from bauxite by treatment with NaOH solution. Solid impurities, including silica and Fe2 O3 , settle out, and Al2 O3
3H2 O can then be crystallized. Heating produces Al2 O3 . Reduction is performed electrolytically on the Al2 O3 dissolved in molten cryolite, Na3 AlF6 , in a cell with carbon electrodes; aluminum metal is produced at the cathode, while the anode is consumed by the oxygen that otherwise would be liberated at an inert anode in an electrochemical process. The net reaction is 2Al2 O3 ‡ 3C ! 4Al ‡ 3CO2

…12-9†

This requires less energy than electrolysis with inert electrodes to produce Al and O2 because of the smaller free energy change involved in the overall process. It is still an extremely energy-intensive process because of the strong AlÐO bond energy that must be overcome. The electrolysis process produces some ¯uoride and other particulate emissions that must be trapped to avoid air pollution problems, but the most abundant waste products of aluminum mining are the insoluble materials from the NaOH treatment, the so-called red mud tailings, and, of course, any waste from the generation of the electricity employed. However, most of

12. THE EARTH'S CRUST

459

the electricity used for aluminum smelters is generated from water power for economic reasons. Per¯uorocarbons (e.g., CF4 ) are produced when the Al content of the electrolysis bath is too low to maintain the reaction, and the voltage rises to cause secondary reactions to take place between the ¯uoride and the electrode material. It has been estimated that 30,000 metric tons of carbon tetra¯uoride and 3000 tons of hexa¯uoroethane are released annually by worldwide Al metal production.5 These are inert, nontoxic materials, but they have signi®cant potential as greenhouse gases (Chapter 3). Because they are resistant to even the highly reactive atoms and free radicals of the upper atmosphere, breakdown is very slow (resulting mostly from photolysis by very short wave-length UV radiation). It is estimated that the lifetime of CF4 in the atmosphere is as long as 50,000 years (Table 5-1).

12.2.6 Gold The recovery of gold has some particular environmental consequences. Gold is usually found in the form of the free metal, but only rarely in the large nuggets of Gold Rush legend. Rather, the gold is in ®ne particles, often very intimately mixed with worthless rock. Because of gold's high density, it can be recovered in some cases by physical separation such as placer mining of river gravels, where weathering processes have released the metal from its original matrix. Such processes on a large scale have major physical consequences because the water system is disturbed through dredging and waste gravel deposition. However, the desire to use less tractable sources, and especially low-grade ores that can be pro®table because of the high value of the metal, has resulted in reliance on some chemical processes that can have more serious environmental consequences. One such process involves the dissolution of the metallic gold in mercury metal, in which it has high solubility. The liquid mercury solution (amalgam) is then easily separated from the debris, and the gold can be recovered by distilling the mercury away. This is a simple technology that can be used in relatively primitive mining operations: for example, the gold mines of the Amazon Basin of Brazil. Unfortunately, when carried out with simple technology, the mercury tends to be condensed relatively inef®ciently, and there are losses to the environment both as the vapor and the liquid, with consequences that were discussed in Section 10.6.7. A somewhat more sophisticated chemistry is involved in a second process that involves the use of cyanide salts. Although gold is a very nonreactive element, it does form strong complexes with some soft ligands (Section 9.5). One of these is cyanide. In the presence of a cyanide salt such as KCN, the gold 5

P. Zurer, Chem. Eng. News, p. 16, Aug. 9, 1993.

460

12.3 SOILS

can be slowly oxidized by air to the soluble K2 Au…CN†4 , which can be leached from the rock and concentrated for gold recovery (see Table 12-3). This process employs large volumes of rock and large amounts of cyanide, with considerable risk of release of toxic cyanide to local water systems. This risk has been realized several times. In late 1999, cyanide from a holding pond at a gold extraction operation in Romania was released into the Tisza River when a dike failed. This river carried the contamination into Hungary and into the Danube. Massive kills to ®sh and other fauna resulted. Six weeks later a dam broke at a similar installation in a tributary upstream of the original release. Pollution involves not only the highly toxic cyanide ion, which is fairly rapidly oxidized to less toxic cyanate, CNO , but also heavy metals, in this case especially copper and zinc, which will remain in the river sediments for a much longer time. This spill is just the latest of several similar examples; 3  106 m3 of solution spilled into the Essequibo River in Guyana in 1995, and 2000 kg of KCN spilled into the Barskoon River in Kyrgyzstan in a 1998 mining truck accident. Cyanide wastes have contaminated several areas in the western United States. 12.3 SOILS Soil, ordinary dirt that we pay little attention to, is a vital substance because it is the basis of much of our food supply. Unfortunately, human activity frequently causes degradation of soil in ways that range from loss of nutrients to changes in the physical character of the soil to contamination with toxic materials to loss of the soil itself. Many agriculturally productive soils are being washed or blown away through erosion as natural vegetation is destroyed. Others in dry areas are being converted to deserts through overgrazing and other activities that exceed the soils' carrying capacity. Much of the tropical land converted to agricultural use through forest clearing is abandoned after a few years. Soil degradation is of serious concern in terms of its impact on future food needs.6 12.3.1 Soil Formation and Composition Surface rocks are subject to breakup and chemical change by a variety of processes called weathering. Some of these processes are listed brie¯y. Physical disintegration of rocks caused by temperature effects, frost, wind, water, and ice erosion. Some of these factors are also responsible for transporting the weathering products away from their original sources. The small particles produced have a large surface area that facilitates other weathering processes. 6

G. C. Daly, Science, 269, 350 (1995).

461

12. THE EARTH'S CRUST

Chemical reactions with water (e.g., hydration or hydrolysis). Hydration is illustrated by reaction (12-10); the change in crystal structure as water molecules are gained or lost will result in disintegration of the material. Hydrolysis involves a more extensive change in the material as shown, for example, in reaction (12-11). Reactions of this sort can liberate cations from the rocks [e.g., K in (12-11)]. 2Fe2 O3hematite  3H2 O ! 2Fe2 O3
3H2 Olimonite ‡

KAlSi3 O8microcline ‡ H2 O ! HAlSi3 O8 ‡ K ‡ OH

…12-10† …12-11†

Attack by acid, especially carbonic acid. Reactions (12-12) and (12-13) are examples of the weathering interactions of acid with minerals. Reaction (1211) could also have been written as an example of acid attack. CaCO3insoluble ‡ H2 CO3 ! Ca…HCO3 †2soluble CaAl2 Si2 O8anorthite ‡ 2H‡ ‡ H2 O ! Al2 Si2 O5 …OH†4kaolinite ‡ Ca2‡

…12-12† …12-13†

Oxidation reactions involving substances in low oxidation states. Reaction (12-14) illustrates a hydrolysis reaction accompanied by oxidation of Fe(II): 12MgFeSiO4olivine ‡ 8H2 O ‡ 3O2 ! 4Mg3 Si2 O5 …OH†4serpentine ‡ 4SiO2 ‡ 6Fe2 O3

…12-14†

Biological effects. These may take the form of physical disruption by plant roots, chemical effects from substances excreted from roots, and bacterial action. For example, the reactions in the nitrogen cycle and the organic materials produced by biological action can determine the soil pH and consequently solubilities and leaching on a local level. The weathering products that result from these various processes depend on the composition of the initial rock and the conditions. Rocks with high silica contents, that is, with more SiÐO bonds, tend to have the greatest chemical stability simply because of the large SiÐO bond energy, and igneous rocks (those produced from molten material), formed under the most extreme conditions of temperature and pressure, are most reactive to weathering decomposition. Igneous silicates high in magnesium and iron (e.g., olivines) produce soluble Mg2‡ and SiO44 and insoluble FeO(OH) under the action of H2 O and CO2 , while feldspars with magnesium, calcium, and aluminum contents give soluble Na‡ , Ca2‡ , and SiO44 , and kaolinite as the insoluble products. However, at nearly neutral conditions (pH 5±8), further dissolution of the silicate component can take place, leading to a residue of Al2 O3
3H2 O, while under more acidic conditions, solid SiO2 is left with soluble Al3‡ species. This last process is of concern as a result of acid rain in view of the toxicity of Al3‡ toward plants (Section 10.6.9).

462

12.3 SOILS

Weathering patterns vary with climate zones. For example, in wet temperate forest regions, decay of organic material produces acidic leaching conditions, so that the upper levels are depleted in FeO(OH) and some alumina, while material with a high silica content is left behind. In tropical rain forest conditions, where temperature and moisture conditions lead to faster decay, conditions are less acidic, and leaching removes more of the silica components, leaving FeO(OH) and alumina clays. This is shown schematically in Figure 12-3.

Rainfall Polar desert and tundra

Northern temperate (Taiga)

Dry grassland and desert

Tropical forest

Temperature

FeOOH + Al2O3 Al2O3 Kaolinite Montmorillonite-Ilite Little alteration Unchanged rock FIGURE 12-3 Weathering products from polar (left) to equatorial (right) regions, showing dependence on temperature and rainfall. Based on P. W. Birkeland, Soils and Geomorphology, Oxford University Press, New York, 1984.

12. THE EARTH'S CRUST

463

The eventual result of the breakup and composition changes of weathering reactions is the formation of soil; this, of course, is the fraction of the earth's surface utilized for plant growth. Soil may be regarded as the upper layer of the regolith, which is the weathered and broken-up material overlying bedrock. Soil is the most heavily weathered portion of the regolith and is normally signi®cantly in¯uenced by plant materials. Soils play an important role in environmental chemistry besides providing a site for plant growth. Much of this role depends on the microorganisms that are important soil components. The absorption of CO has already been referred to, as have the carbonate equilibria (Section 9.2.2), which in soils are strongly dependent on CO2 generated from bacterial degradation of organic materials. Other processes include rapid SO2 absorption; soils have been shown to be effective in removing SO2 from the air. Buffering of pH, and of metal ion concentrations, are also important aspects of soil chemistry. A typical soil contains stones and gravel, coarse and medium-sized material such as sand and silt composed of silica and other primary minerals, and ®ner weathered material classed as clays. Most soils contain a few percent organic components such as humic substances (Section 9.5.7) and undecomposed plant materials, although a few organic soils (peats, mucks) may contain up to 95% organic matter. Typical soils exhibit several layers (horizons) of somewhat different composition that are important in soil classi®cation. These horizons are the result of biological decay, weathering, and leaching processes. An idealized version is shown in Figure 12-4. Soils play a signi®cant role in the carbon cycle (Section 10.2), with about 60 billion tons of CO2 released annually from soils. About the same amount is bound into land plants. Much of the CO2 release comes from decomposing plant litter in the upper layer, but about two-thirds is released at deeper layers, from respiration in roots, fungi, and soil microorganisms. Carbon dioxide partial pressure in soils can be high. Factors that enhance microbial activity, which converts organic matter to CO2 , in¯uence the amount of organic matter a particular soil will retain. Thus, temperate regions with cold winters allow a signi®cant buildup of organic constituents, while tropical regions with yearround warmth promote microbial decay and often produce soils with little organic material below the upper layer of debris. The size and the nature of the ®ne particles in the soil are the most important determinants of its chemical and physical properties, although the organic constituents can have a major in¯uence as well. The voids or pores between the particles are important reservoirs for soil gases and soil moisture; large diameter pores allow water to drain, while small diameter pores retain water. Some clays swell when wet, as water molecules enter the crystal lattice. As a consequence of shrinkage on drying, such soils tend to crack. At the same time, the soil may cake and become impervious to moisture. Cohesion of the clay particles, which is also dependent on moisture and sodium ion content,

464

12.3 SOILS

A

Loose organic matter Partially decomposed organic matter Maximum organic material

Maximum leaching; minimum clay, organic material B

Maximum accumulation of silicate or oxide clays

C Broken up/partially changed parent minerals

D Bedrock

FIGURE 12-4 An idealized soil pro®le: A, B, C, and D are typical horizons (sometimes designated by other letters); they may be further subdivided, A1 , A2 , etc. An initial ``O'' horizon is often indicated.

determines the stickiness of the soil and its agricultural workability. The clays also are largely responsible for the very important ion exchange properties of soils, although humic materials contribute signi®cantly. Typical clays are aluminosilicates, present largely as colloidal particles; that is, the size is less than a micrometer. The particles are composed of layers or sheets somewhat analogous to the structure of graphite. The surface area of such small particles is very large and, in addition, internal area between the layers may be available to bind other materials. Thus, surface properties and adsorption are quite important. A variety of clays is recognized; two that are common components of soils are kaolinite and montmorillonite, the formulas for which are (idealized and simpli®ed) Al2 Si2 O5 …OH†4 and NaMgAl5 Si12 O30 …OH†6
nH2 O, respectively.

465

12. THE EARTH'S CRUST

The structure of aluminosilicate clays is based on tetrahedral SiO4 units, each of which shares three of its oxygens with other tetrahedra to produce a planar sheet. If this layer is taken as in®nite, the stoichiometry is Si2 O2 5 . Associated with this is a layer of octahedral AlO6 units that share the apicial oxygens from the SiO4 units in the tetrahedral layer. The octahedral unit can be written AlOn …OH†m , where n oxygens are shared with Si, and m OH groups bridge the aluminum atoms. Kaolinite (Figure 12-5) has an equal number of Si and Al atoms, and the combined layers are neutral. This combined layer is bound to others in the crystal by hydrogen bonds. In pyrophyllite, AlSi2 O5 …OH†, a second layer of SiO4 tetrahedra is bound by sharing of the corner oxygens to the other side of the octahedral aluminum layer, giving a sandwich-type structure. These layers are held to others in the solid by van der Waals attractions. In both types of clay the layers are comparatively easily separated. If some of the trivalent aluminum atoms are missing or replaced by bivalent ions such as Mg2 orFe2 , the charge balance is no longer maintained. The layers carry a net negative charge, which is balanced by other cations between the layers. These additional cations also serve to hold the layers together by Coulombic attraction. In some layered structures, the interlayer cations, which may be Na , K , or Ca2, produce a fairly strong attraction between the layers, although they can still be separated readily. This class of material is known as mica; an example is muscovite, NaAl3 Si3 O10 …OH†2 . In other structures with lower charges on the layers, the interlayer cations hold the layers together more weakly; the ions themselves may retain their hydration sheaths, and there are water molecules between the layers. This is the case for montmorillonite (Figure 12-6). Because the water molecules between the layers can be removed or added easily, such clays show marked changes in volume upon wetting or drying. These clays are referred to generally as smectites.

= Si = Al =O

FIGURE 12-5 The structure of kaolinite. This is based on a two-dimensional layered structure of SiO4 units (Figure 12-1g) perpendicular to the page; only three oxygens are shown around each Si for clarity. The geometric arrangement is shown schematically on the left.

466

12.3 SOILS

Na+, n H2O = Si = Al/Mg =O

FIGURE 12-6 The structure of montmorillonite. The silicate sheet structure similar to Figure 12-1g is perpendicular to the page; for clarity only three oxygens are shown around each Si. The geometric arrangement is shown schematically on the left.

Some soils, particularly in the tropics, contain colloidal metal hydroxides such as Al…OH†3 and FeO(OH) that are also referred to as clays and have similar properties. The structure of the aluminum hydroxide particles is based on Al3 ions occupying the octahedral holes between two close-packed layers of OH ions, similar to the aluminum layer in the silicate clays described earlier. The layers are held together by van der Waals forces. Clays are capable of entering into ion exchange reactions in two ways. First, H ions can be lost from the OH groups, and replaced by other cations (which may later be exchanged for still other cations). This activity is pH dependent. Second, interlayer cations may be exchanged. Ion exchange is discussed in more detail in Section 9.7. The colloidal-sized clay particles can pack together to give a low-porosity soil that has low permeability; that is, water has considerable dif®culty ¯owing through it. A layer of clay can be quite effective in preventing the passage of groundwater, with the possibility of protecting a deep aquifer from contamination by polluted surface water, but also preventing its recharge. Impermeable clay layers are an important feature of a well-designed land®ll (see Section 16.2), being used both as a cap to keep water out and as a liner to restrict contaminated leach water, which may enter the ®ll through imperfections in the cap, from seeping into the groundwater. Hydrated metal oxide clays of Fe and Al that dominate some tropical soils and are also present in colloidal form in other soils have ion exchange properties similar to, but weaker than, those of the aluminosilicates. They tend not to be as sticky and adherent as the silicates, and soils with high proportions of hydrous oxide clays can be cultivated under moisture conditions that

467

12. THE EARTH'S CRUST

make siliceous clays unworkable. They can become concretelike when dry, however. Every soil is assigned to one of a variety of classes. Although the details of soil classi®cation are beyond the scope of this book, Table 12-4 gives some of their characteristics.

TABLE 12-4 Soil Typesa Name

Description

Entisols

No horizon formation, little organic matter; includes sandy areas, thin soils on rock, recently produced soil deposits. Mostly used as grazing land in dry areas; can be productive in humid areas. Have been called lithosols and regosols.

Vertisols

High content of swelling clays; crack extensively on drying. Large areas in India, Australia, Sudan; very dif®cult to farm. Have been called grumusols.

Inceptisols

Young soils without much weathering.

Aridsols

Found in arid regions, they have had little leaching. Upper layers tend to be neutral or basic; lower levels contain calcium carbonate and often soluble salts. Many deserts are of this type; with irrigation, they can be very productive.

Spodosols

Temperate region soils from humid, forested areas; they are highly weathered and leached. Found in large areas in northeastern North America, northern Europe, and Siberia. Productive if fertilized. Many have been called podzols.

Al®sols

Less weathered than spodosols, but also temperate, humid region soils formed under less acidic conditions because of different vegetation, especially deciduous forests. They are widely distributed worldwide and are generally excellent agricultural soils.

Mollisols

High nutrient and organic content, generally formed with grassland vegetation in temperate regions with moderate rainfall. Major areas are the Great Plains of North America, eastern Europe to the Urals, northern China, and South America. Very fertile.

Oxisols

Highly weathered and leached, with few nutrients; found in tropical forests, especially in South America and Africa. They have been called latosols and laterites.

Histosols

Very high organic content, water-saturated soils, found, for example, in bogs. When drained, they can be very productive.

a

Soils are classi®ed into a large number of types and subtypes. Classi®cation systems have been based on how soils were formed (or thought to be formed) or on soil properties: texture, color, composition, moisture, and others. The presence or absence of certain horizons (layers) in the soil pro®le are important aspects of the classi®cation scheme. This table gives the main soil types and some of the older equivalents.

468

12.3 SOILS

Acid leaching, also called podzolization, one of the most important natural processes occurring in soils that determines their properties and agricultural characteristics. The process occurs most markedly in soils of moist, forested, temperate, and cold regions, such as the northeastern United States. The top layer of such soils consists of organic materials containing relatively few metal ions. As these materials decompose, acids are formed that are washed into the levels below. As a consequence, the soil beneath the organic layer is leached of most minerals except those with a high silica content. Aluminum and iron oxides and organic matter are precipitated in the lower layers, as soluble material and noncoagulated colloids are washed down. Such soils contain few nutrients except in the upper organic layers, the nutrients having been leached out of the levels beneath the surface. These soils are suitable for deeprooted plants such as trees, but used agriculturally, they soon lose fertility. Besides true spodosols, many soils exhibit partial leaching (partial podzolization) when they have less organic matter on the surface and therefore, there is less acid leaching. In wet, tropical forests, oxidation of the organic material is more rapid, and leaching is less acidic than in temperate regions, but very extensive. Silica and montmorillonite types of clay are removed under these less acid conditions, but iron and aluminum oxides remain, giving the soil a red or yellow color. Often deposits of these oxides form near the water table. Upon drying, these may form very hard materials that cannot be cultivated. Such levels are called laterites; the soils are called latosols or oxisols. They are common in much of South America and Africa. Modern farming techniques on such soils are effective only with extensive application of costly fertilizers. Because of this, much tropical land cleared for agriculture becomes converted to pasture after a few years. Both spodosols and oxisols must receive large amounts of fertilization if they are to be useful for large-scale agriculture. With the latosols in particular, modern agricultural methods must be applied with great care to ensure that erosion does not expose the hydrous oxide layer, which could dry out, leading to irreversible loss of agricultural use of the soil. Indeed, primitive agricultural practices on many tropical forest lands, while not highly productive overall, display an excellent adaptation to the chemical nature of the soils. These methods have been the ``slash and burn'' type. Small ®elds are cleared of vegetation by burning. This converts the nutrient material in the growing vegetation to inorganic salts that provide a high level of fertilization for crops for a few growing seasons. When these nutrients are used up, the ®eld is allowed to return to forestation for a few years, until the process can be repeated. Soils with less abundant vegetation and less rainfall (called aridsols) have correspondingly less acidic leaching, and in fact may be neutral or basic. Calcium carbonate occurs at modest depths or even near the surface (calcar-

469

12. THE EARTH'S CRUST

eous soils), there may be soluble salts present, and the nutrient content is often very high. Some of these soils can be highly productive if irrigated. Slightly acid to neutral soils are favored by many cultivated crops, and although some plants prefer strongly acid soils, it is often necessary to increase the pH of agricultural, garden, and lawn soils by the addition of lime. Agricultural limes are impure forms of calcium oxide, calcium hydroxide, or calcium carbonate, usually with considerable Mg present. Limestone and dolomite are common sources. On the other hand, if necessary, the acidity of the soil can be increased by the addition of sulfur, which is oxidized to H2 SO4 by soil organisms. Many fertilizers (Chapter 10) increase soil acidity also, for example by reactions such as ‡ NH 4  2O2 ! 2H ‡ NO3 ‡ H2 O

…12-15†

The need for fertilization of soils has already been referred to, and several of the major fertilizers that are needed were discussed in Section 10.5. Phosphorus, nitrogen, and potassium are considered macronutrients, while many other elements are necessary micronutrients. Of the macronutrients, phosphate may be present in the soil as insoluble phosphate salts that form as a result of the reaction between the hydrogen phosphate ions with metal ions (chie¯y, Fe, Al, Ca, either free or held in the clays) or with hydrous oxides. Reversible ion exchange reactions also may retain phosphate, for example, as in reaction (12-16): Al…OH†3 ‡H2 PO4 ! Al…OH†2 H2 PO4 ‡ OH

…12-16†

Phosphate held in this way is more readily available than that of the insoluble phosphate salts. Nitrogen may be present as nitrate, which is held only weakly by anion exchange, or as the ammonium ion, which can be held by cation exchange with the clays. The potassium ion is nearly the same size as the NH‡ 4 ion, and is held in the same way. Weakly held nutrients are easily leached away, and much of the nitrogen applied as fertilizers can end up in lakes and streams rather than on the ®eld. Micronutrients, especially metal ions, may be available in clays or other insoluble mineral forms. In some instances one or more such nutrients, although present, may be unavailable to plants because they are in insoluble forms, and some metal ion de®ciencies have been relieved by treating the soil with complexing agents of the EDTA and NTA types that can solubilize these materials as complexes (Chapter 9). Some input of micronutrients such as chloride and sulfate comes from rainwater. 12.3.2 Contaminated Soils Contamination of soils is an important concern. Contamination by pollutants can come from water leaching from land®lls and waste dumps, spills and

470

12.3 SOILS

residues from industrial operations of many kinds, leaking storage tanks, and so forth. A contaminant may be mobile through solution in soil water, as a water-insoluble liquid, or to a lesser degree through volatilization in the soil. Contaminants in the form of dusts may also be spread by wind, but these remain on the surface unless other mechanisms are involved. Water-soluble contaminants, which can be either inorganic or organic, will ¯ow with the water in which they are dissolved, but generally not at the same rate. Adsorption to soil components will slow the motion of dissolved materials to an extent determined by the partitioning of the substance between the water phase and the solid. If a soluble pollutant is injected into the soil at a point source, as the adsorption capacity of the soil is exceeded the pollutant will follow the ¯ow of groundwater (advection) but will also spread laterally through processes of dispersion. These can involve diffusion, but are largely the result of ¯ow inhomogeneities. The concentration of the pollutant will decrease with distance from the source, as a result of adsorption and spreading. Because some of the contaminant will inevitably be left behind and will be released only very slowly, the contaminated region always extends to the source, even for a single spill event that seems to ``sink in.'' Some of this may be taken up by later rainwater to provide a long-term input of pollutant into the groundwater. A water-insoluble liquid, on the other hand, will ¯ow as a separate phase. However, there will always be some solubility, even of organic liquids generally considered insoluble. The undissolved material will behave differently depending on whether it is heavier or lighter than water. In either event, a liquid spill will descend (and spread) until it reaches the water-saturated zone (Figure 12-7). The lighter liquid will ``¯oat'' on the water layerÐthat is, it will occupy a zone above the saturated region. The heavier liquid, on the other hand, will pass through the water level until it reaches the impervious bed on which the water rests. The details of this process are by no means simple. Globules of liquid may also remain in the water-saturated region. Through these globules and by pooling below the water level for the heavier liquid, or by ¯oating on the water surface for a light one, a continuous reservoir is provided to contaminate the water through solubility. The heavier liquid may also enter cracks, pores, or capillaries in the soil or rock and remain strongly held. This too may be released slowly into the water phase through solution. A lighter liquid may also have some ability to diffuse as a vapor into soil above it. It is frequently desirable to treat polluted soil to prevent the pollutants from spreading or to recover a site for safe use.7 Remediation approaches may be removal of the pollutant, or its stabilization in a form that is immobile and 7

John K. Borchardt, `Dealing with soil contaminants', Today's Chem. Work, 4(3), 47 (March, 1995).

471

12. THE EARTH'S CRUST

A

B

Soil

Direction of flow

Ground water

Impermeable layer FIGURE 12-7 Schematic illustration of the behavior of spills of heavy (A) and light (B) insoluble liquids.

inert. One approach to soils in which the pollution is in the soil water is to drill wells to intercept the water and pump it out for treatment. This practice can be effective in reducing the water concentration of the pollutant while pumping is continued, but on cessation, water levels of the contaminant usually rise again as the more strongly held material is continually and slowly released. At any rate, this is a long-term treatment procedure. Injection of detergent solutions to help release organic materials may provide more ef®cient removal. Volatile contaminants may be removed by vapor stripping. Air is drawn from holes bored in the soil to carry vapors out where they are trapped. This can be enhanced by injecting hot air or steam. Such treatments are unlikely to remove all the contaminating materials, but they can reduce the concentration signi®cantly, perhaps to safe levels, and can minimize the area of spread by reducing the concentration gradient that drives diffusion. (The remaining material will continue to spread in all directions by diffusion, subject to holdup by adsorption.) Stabilization consists of using a chemical reaction to incorporate the contaminated soil into an inert solid from which the contaminant will not be released at a signi®cant rate through leaching or other natural processes. As part of this, the contaminant may undergo a reaction, or it may simply be physically encapsulated, depending on its nature. This can be carried out directly on the soil in situ if contamination is close to the surface, or excavation

472

12.3 SOILS

may be used. The approach is also useful in dealing with sludges from stack gas scrubbing or other industrial processes to make land®lling safer. The soil (or sludge) is mixed with materials that react to solidify to a nonreactive solid. Most used are portland cement, alone or mixed with ¯y ash or silicates, lime± ¯y ash, and cement or lime kiln dust. Another solidi®cation=stabilization technique that has been proposed is in situ vitri®cation, in which electrodes are inserted into the soil and a high current passed between them. Ohmic heating causes the soil to melt, pyrolizing some contaminants and trapping others in the glassy residue that forms on cooling. Metals whose compounds are environmentally benign have been used with excellent results to reduce both organic and inorganic contaminants.8 Iron is the usual choice, but zinc and tin are alternative possibilities. In this method, a porous barrier of metal ®lings is put in place to intercept the groundwater ¯ow. Many organochlorine compounds undergo reaction: Fe  RCl  H ! Fe2‡ ‡ RH ‡ Cl

…12-17†

The result is a much less toxic product. Other inorganics such as dyes and pesticides can also be reacted in a similar manner. Inorganic materials such as Cr(VI) can be reduced to less dangerous, immobile forms. The signi®cant installation cost is offset by essentially zero operating costs. Metal reduction can also be used in aboveground treatments. Excavated soils can also be cleaned by washing with appropriate reagents, or organic contaminants can be burned off by heating. Bacterial degradation of organic pollutants is receiving more and more interest as a remedial process that can take place in situ as well as in excavated soil.9 The maintenance of optimum conditions for bacterial growth, including nutrient supply, can be a problem. Bacteria can also be helpful in metalcontaminated soil by converting one chemical species to a less dangerous one, or concentrating the metal in the biological mass for recovery. Another biological process, phytoremediation,10 is applicable to metal ions in particular; this process uses plants that accumulate metal ions from soils in which they grow. Although plants generally take up metal ions from soils, some, called hyperaccumulators, can take up unusually large amounts of particular elements. A variety of metal ions, including copper, nickel, and lead, and some nonmetals such as selenium, can be taken up, in some cases by as much as 5% by weight of dry plant material. The metals can be concentrated in the ashes on incineration for recovery or safe disposal. This process appears to be applicable to shallow contamination (perhaps up to a meter) that can be reached by the plant roots. Development has just begun. 8

E. K. Wilson, Chem. Eng. News, p. 19, July 3, 1995. D. R. Lovley, Science, 293, 1444 (2001). 10 A. S. Moffat, Science, 268, 303 (1995); A. M. Rouhi, Chem. Eng. News, p. 21, Jan. 13, 1997. 9

12. THE EARTH'S CRUST

473

Soil remediation is a rapidly growing ®eld, with many approaches available. Clearly, the best will depend on the speci®c problem to be solved. As more experience is gained with these remediation methods, ef®ciency and costeffectiveness should improve considerably.

12.4 NONMETALLIC MATERIALS FROM THE EARTH Many nonmetallic inorganic materials are obtained from the rocks and minerals of the earth. Some of these are employed with little treatment, while others undergo considerable chemical modi®cation before use. The environmental problems associated with these substances are chie¯y those associated with mining or quarrying and crushing of large volumes of rock or clay: that is, with destruction of landscape and emissions of particulate materials into water and the air. The common minerals involved are not considered to be toxic, but the physical form in which the particulates are emitted can render them harmful to health. In the remainder of this chapter, we shall consider brie¯y a few aspects of some of the more important examples of substances of this class.

12.4.1 Stone From the beginning of civilization, stone has been used as a material of construction. Marble, limestone (carbonates), sandstone, and granite (silicates) are examples of widely used building stones. Like other rock, the stone used for construction is subject to weathering processes and particularly to attack by acid constituents of urban airs. Sulfur and nitrogen oxides, which they form strong acids upon hydrolysis, are the primary acid components involved. Attack is particularly severe on carbonate stones. It is well known that many stone buildings and carvings that have existed for centuries have undergone rapid and extensive deterioration in modern times as air pollution from industrial and urban sources has increased and the acidity of the precipitation has led to faster deterioration. Attack can involve the acid rain itself, but dry deposition involving dissolution of gaseous pollutants in the ®lm of moisture, which can condense on the surface of the stone may also do a great deal of damage. While much of the weathering attack on building stone is due to acid attack from H2 SO4 arising from SO2 emissions and to carbonic acid, water itself can be destructive if it enters the pores in the surface layers of the stone and causes the surface layers to ¯ake off through stresses imposed in freezing and thawing. The most serious cause of surface disintegration of this sort, however, is the strain imposed just beneath the surface by recrystallization of salts as water

474

12.4 NONMETALLIC MATERIALS FROM THE EARTH

enters and evaporates from the pores. Any source of a salt having signi®cant water solubility (e.g., sea spray) can contribute to this, but in general calcium and magnesium sulfates formed from the acid attack of industrial air [reaction (12±18)] are probably most important. CaCO3  H2 SO4 ! CaSO4 ‡ H2 O ‡ CO2

…12-18†

That is, air pollution does not just dissolve the stone from the surface, but can also cause layers a few millimeters thick to disintegrate. In many places, attempts are under way to protect stone monuments and historical buildings from deterioration from these causes.11 Protective measures were undertaken as long ago as the ®rst century b.c. when workers rubbed wax on the warmed stone. Various waxes, resins, silicones, and other materials have been applied more recently. Such treatments rarely achieve deep enough penetration to be effective; water can get behind a thin ®lm and eventually cause the treated layer to ¯ake off. Some use is being made of polymers in processes where solutions of monomers of good penetrating power are applied to the stone, followed by in situ polymerization. Acrylics, epoxies, and alkoxysilanes are among the materials used. Another treatment for carbonate stones involves the deposition of BaSO4 in outer layers of the stone. Much less soluble than CaSO4 or MgSO4, this material forms solid solutions with CaSO4 . Consequently, the strains introduced through the recrystallization process are much reduced.

12.4.2 Clay-Based Materials Clays are among the oldest technological materials, used for bricks and ceramics from prehistoric times. Bricks for building purposes have been prepared simply by drying clays or muds. The hydrous oxide layers of lateritic soils are one example of soil that provides a good building material by simple drying, although generally aluminosilicate clays will produce a stronger and more permanent substance by ®ring. Brick, tile, and pottery are all made in this way. A nonswelling clay is required that can be formed into the desired shape as a paste with water and does not deform signi®cantly on drying. The ®ring process causes changes in the chemical nature of the aluminosilicate and permits the individual particles of the clay to fuse together to produce a hard, strong structure. This is essentially irreversible; water will not reconvert the ®red material to soft clay, as it will after simple drying. The ®red clay is porous, but a nonporous surface can be achieved by a glaze of material that is melted to a glass. 11

C. Wu, Consolidating the stone: New compounds may protect statues and buildings from weather damage, Sci. News, 151, 56 (1997).

475

12. THE EARTH'S CRUST

12.4.3 Glass Glasses are rigid, noncrystalline materials that are often called supercooled liquids, but a glass is in fact a separate physical state. It is like a liquid in having a nonrepeating structural pattern, but it is a rigid structure without molecular mobility. In spite of the widely held belief, long standing does not cause glass to ¯ow, and if old window panes are thicker at the bottom, it is because old glassmaking techniques produced glass that was not of uniform thickness and the panes were installed that way. There is a glass transition temperature, above which the material transforms into a true supercooled liquid of high viscosity. Common glass (soda glass) is a silicate, but it does not correspond to a particular compound. Silica, SiO2 , is a three-dimensional network based on SiÐOÐSi linkages. If the atoms are arranged in a regularly repeating pattern, a crystalline form of quartz is produced, but they may be arranged irregularly, forming a glass. Addition of an oxide of a metal with a small tendency to form a covalent bond to oxygen (e.g., Na2 O) to SiO2 results in breakage of the Si±O±Si links: Na2 O ‡

Si

O

Si

!

Si

O ‡

O

Si

‡ 2Na‡

…12-19†

As a result, the properties of the network structure are changed and the softening temperature is lowered. These properties can be controlled by appropriate selection of the composition of the glass. Addition of B2 O3 will result in SiÐOÐB linkages, since boron also has a strong af®nity for oxygen. This is the basis of the borosilicate glasses of which Pyrex12 is an example; they have higher softening temperatures and smaller coef®cients of thermal expansion than the soda glasses. Lead oxide produces a high index of refraction and is used in ``crystal'' glassware. As discussed in Chapter 10, some of this lead can be leached out of the glass with use. Common glass is made from SiO2 , Na2 O, and some CaO, which are fused at high temperatures. The source of the Na2 O and CaO may be the carbonates or other salts that decompose to oxide upon heating; SiO2 is obtained as sand. There are restrictions on the purity of the starting materials, since many metal ions and colloidal metals, sul®des, and selenides produce colors in the glass. Indeed, this is how colored glasses are made. Scrap glass can easily be used in the melt (Section 16.17.1), but the need to sort the glass from contaminants and to separate the colored glasses causes problems in recycling. To produce a product with acceptable speci®cations, the starting materials must conform to appropriate compositions. For economic reasons, much recycled glass is used in products that do not depend very much on the glass properties, such as ®llers in asphalt (``glasphalt''). 12

Trademark of the Corning Glass Company, Corning, New York.

476

12.4 NONMETALLIC MATERIALS FROM THE EARTH

12.4.4 Cements Use of brick and stone for construction requires a cement or mortar to bind them together. A cement is the binding material, in this context a powder activated by water. If sand is added as a ®ller, the mixture is called a mortar. Mortars are used in bonding bricks, and other building units. Mixtures with coarse materials such as gravel or crushed rock are called concrete. Use of cements goes back to antiquity, with various substances having been used. The earliest cements were based on gypsum, CaSO4
2H2 O, which can be dehydrated to plaster of paris at temperatures near 2008C: CaSO4
2H2 O ! 3=2H2 O ‡ CaSO4
1=2H2 O

…12-20†

Upon mixing with water, the reaction can be reversed, and the material will set to a hard mass. Plaster of paris has some uses even today. It evidently was used with sand as a mortar for masonry by the ancient Egyptians, but gypsum is slightly water soluble and unsuited to moist climates. Lime mortars were also discovered quite early in the development of civilization. These are formed by heating (calcining) calcium carbonate, and slaking the quicklime (calcium oxide) produced with water to give slaked lime, calcium hydroxide: H2 O

CaCO3 ! CO2 ‡ CaO ƒƒƒƒƒƒ! Ca…OH†2

…12-21†

Ca…OH†2 ‡CO2 ! CaCO3 ‡ H2 O

…12-22†

A paste of slaked lime, sand, and water can be used as a plaster on walls or as a mortar; it hardens by chemical reaction with atmospheric CO2 :

Lime mortars have two disadvantages. First, they depend on diffusion of CO2 from the air into the interior of the mass, and consequently they cure slowly and not always completely. Second, they will not harden if contact with water occurs. Hydraulic cements, those that will harden in the presence of water, ®rst were made by mixing volcanic ash with lime. When mixed with water, these so-called lime±pozzolana cements, harden by a chemical reaction that produces calcium silicates and aluminosilicates from the calcium hydroxide, silica, and alumina. The last two are provided by the volcanic ash. Limestone containing considerable clay also produces hydraulic lime upon calcining; other similar reactions can take place. These materials were the forerunners of portland cement, the material now in general use for construction purposes. Portland cement is chie¯y composed of calcium silicates and calcium aluminosilicates; the primary compounds in it have the empirical formulas 3CaO
SiO2 , 2CaO
SiO2 , 3CaO
Al2 O3 , and 4CaO
Fe2 O3
Al2 O3  The CaO is ordinarily obtained from limestone and the SiO2 , Al2 O3 , and Fe2 O3 from clay

12. THE EARTH'S CRUST

477

or shale, although blast furnace slag, fuel ash from power plants, and industrial calcium carbonate wastes are sometimes employed. The starting materials are ground and heated to incipient fusion. All water and CO2 is thereby removed, and chemical reactions to form the silicate and aluminate compounds take place. After cooling, the solid residue, called clinker, is ®nely ground with gypsum. When water is mixed with the cement, complex reactions take place which involve hydration of the compounds present and the formation of new compounds. It is these chemical hydration reactions that are responsible for the hardening of the cement. These curing reactions are not completed for weeks, although they are fast enough to cause the paste to become solid in a matter of hours. Cement is produced in kilns that are sloping, rotating cylinders, typically several hundred feet long, heated to 1500±20008C by burning coal or oil at the lower end while the raw materials are added at the other. Normal operation releases carbon dioxide, nitrogen oxides, sulfur dioxide, and particulates. Trapping and disposal of the latter is in itself a problem. Because at the temperatures and long residence times involved, these kilns offer an attractive environment for the combustion of hazardous organic wastes, they are widely used for this; complete destruction of organic molecules is expected to take place. Combustion by-products such as heavy metals and chlorides, for example, are incorporated into the clinker and immobilized. This process has considerable economic advantage for the kiln operator in terms of fuel costs, but there is opposition to such use because of fear of incomplete combustion and possible leaching of toxic heavy metals from the cement, although leaching tests have indicated that the product is safe. Some of the concern stems from the regulations that govern the burning of hazardous waste in cement kilns, which are considerably less stringent than those imposed on regular hazardous waste incinerators (Section 16.5).

12.4.5 Asbestos Several different aluminosilicate minerals are called asbestos (Table 12-5). The term refers to a crystal form or habit that many minerals can exhibit, but only three make up the deposits having important use as commercial asbestos materials. The characteristic of this crystal habit is its ®brous form. The crystals grow in a ®ne, whiskerlike structure with considerable strength and ¯exibility. All are based on shared SiO4 tetrahedra, but some (amphiboles, Figure 12-8) are based on double chains of linked tetrahedra with the double chains linked to each other by interactions with cations. Others (chrysotiles) are based on double layers of SiO4 units similar to the structure of kaolinite (Figure 12-5) but with Mg instead of Al. However, the layers are not ¯at but rolled into cylinders. Again, other ions link the units together. In the bulk, both

478

12.4 NONMETALLIC MATERIALS FROM THE EARTH

TABLE 12-5 Types of Asbestos Name

Properties and comments

Formula

Chrysotile (white asbestos)

A serpentine; most widely used asbestos (> 90%); strong but friable ¯exible white ®bers, less acid resistant than other types

Mg3 Si2 O5 …OH†4

Crocidolite (blue asbestos)

An amphibole; some commercial use ( 83 are radioelements. Some of the radioisotopes of the elements polonium (Z ˆ 84) through uranium (Z ˆ 92) are members of three naturally occurring families or series discussed in Section 13.4.1. The transuranium elements, those beyond uranium in the periodic table, that have been synthesized at the time of writing are 93 Np (neptunium), 94 Pu (plutonium), 95 Am (americium), 96 Cm (curium), 97 Bk (berkelium), 98 Cf (californium), 99 Es (einsteinium), 100 Fm (fermium), 101 Md (mendelevium), 102 No (nobelium), 103 Lr (lawrencium), 104 Rf (rutherfordium), 105 Db (dubnium), 106 Sg (seaborgium), 107 Bh (bohrium), 108 Hs (hassium), 109 Mt (meitnerium), 110 El, 111 El, and 112 El, where El represents an unnamed element. Creation of elements 116 and 118 was announced in 1999, but the announcement was retracted in 2001 because repetition of the experiment in the same and in other heavy element research laboratories failed to con®rm the initial results. The actinium series ends with lawrencium. Seaborgium has been shown to have the chemical properties of molybdenum and tungsten, bohrium those of technetium and rhenium, and hassium those of osmium. Neptunium and plutonium also are produced in trace amounts in uranium ores by the reaction of 238 U with neutrons. This reaction is discussed in Section 13.6.3. Figure 13-1 shows the relationship between the number of neutrons and the number of protons in the stable nuclei. For the ®rst 20 elements (through Ca), N is equal to or very close to Z and the data follow the line labeled (Z ˆ A Z). Beyond 20 Ca, the stable nuclei contain an excess of neutrons and the excess increases with increasing Z. The number of stable isotopes varies from one for many elements to 11 for 50 Sn.2 A radionuclide, A, that decays into a product nuclide B with a change of Z can be represented by a point that is either above or below the stability band in Figure 13-1, depending on the mode of decay. As A decays, the point will move toward the stability band and will be within the band if B is stable. If A is the ®rst member of a radioactive series, [reaction (13-21) in Section 13.4.1], the point representing the last member will be in the band.

2 Nuclides with 2, 8, 20, 50, or 82 protons or neutrons or 126 neutrons are characterized as having a magic number of nucleons. Such nuclides have several distinguishing properties (e.g., high abundance, a large number of stable isotopes, high stability). The correlation between magic numbers and nuclidic properties provides the basis for the shell model of nuclei. In this model, the magic numbers correspond to the number of protons in closed shells of protons or neutrons in closed shells of neutrons. A region of relative stability of superheavy radioelements has been predicted for nuclei close to those with 114 or 126 protons and those with 184 neutrons.

486

13.2 THE ATOMIC NUCLEUS

140

82 126 120

50

82

=

A

–

Z

80

60

Z

Number of neutrons (A–Z)

100

50

28 40

20 28

20

20

8 2

8 2

0 0

20

40 60 Number of protons (Z)

80

100

FIGURE 13-1 Numbers of protons and neutrons in stable nuclei. Magic numbers (see footnote 2) are indicated. Redrawn from S. Glasstone and A. Sesonske, Nuclear Reactor Engineering, 4th ed., Vol. 1, Chapman & Hall, New York. Copyright # 1994. Used by permission of Kluwer Academic Plenum Publishers.

487

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

At least 32 of the 91 naturally occurring elements (including the recently discussed plutonium, 244 Pu) have one or more naturally occurring radioisotopes and 10 have no stable isotopes.3 Furthermore, all 91 elements have one or more (up to 36) anthropogenic radioisotopes. The nuclidic mass (rest mass), M, is expressed on a relative scale based on the mass of an atom of the stable isotope of carbon 12 C, which is de®ned as having a mass of exactly 12.00000000 atomic mass units (amu).4 For example, the values of M for stable 13 C and radioactive 238 U are 13.00335483 and 238.050785, respectively.5 As discussed in the next section, the nuclidic mass is less than the sum of the rest masses of Z hydrogen atoms and N neutrons by an amount equal to the mass-equivalent of the binding energy that holds the nucleus together. The two stable isotopes of carbon, 12 C and 13 C, have experimentally determined isotopic abundances of 98.90 and 1.10 at. %, respectively. By calculating the weighted average of the two isotopic masses, one obtains 12.011 for the atomic weight of carbon. In addition to mass, the nucleons confer other properties on an atomic nucleus. One of the properties is nuclear spin, which is analogous to the spin assigned to an atom based on the orbital angular momentum and the intrinsic spin of the atom's electrons. (See Appendix A, Section A.2.) The properties of a nucleus are consistent with each nucleon having a quantized orbital angular momentum l, an integer value, and a quantized intrinsic spin angular momentum s ˆ 1= 2. When combined, the total nuclear angular momentum or nuclear spin j of a nucleon has a half-integral value. Nuclei with even mass number have a total nuclear spin I equal to 0 or an integer; those with odd mass number have I ˆ half-integer.

3 The number of known naturally occurring radionuclides that decay exceedingly slowly increases as radiometric measurement techniques are improved. New, manufactured radionuclides also are being discovered as the products of nuclear reactions in which high-energy, heavy ions (e.g., 238 U ions) strike a target consisting of an element such as lead and as the products of reactions used to produce new heavy elements. 4 The atomic mass unit is for the neutral atom, not for the nucleus alone. As de®ned, one amu (1 dalton) has a mass of 1=12 the mass of one atom of 12 C, that is,

5




12:000000  10

3

 kg=12

1 ˆ 1:661  10 6:02  1023

27

kg

Values of M and abundances of naturally occurring isotopes and values of M for radioisotopes of the elements are readily available in handbooks. In some tabulations values of D, the mass excess, rather than M are given. The mass excess is de®ned in terms of the isotopic mass M and the mass number A, which is the whole number nearest M, by D ˆ M A.

488

13.2 THE ATOMIC NUCLEUS

13.2.2 Physicochemical Effects of Nuclear Mass and Spin 13.2.2.1 Mass

The physical properties, such as density, viscosity, melting point, vapor pressure, spectra, and rate of diffusion, and the chemical properties, such as reaction rates and equilibrium states, of a given chemical substance are slightly different for isotopomers (chemical species differing in isotopic composition). For example, the normal melting and boiling points of D2 O (2 H2 O, heavy water) are 3.828C and 101.428C, respectively. This is an example of the isotope effect, which increases in magnitude with increasing DM=M, the relative mass difference for two isotopes, and is, therefore, most pronounced for the light elements H, Li, Be, C, N, O, Si, S, and Cl. Even so, the isotope effect is suf®ciently large to serve as the basis for methods of isotope separation (enrichment) for many elements, including uranium. An important mass-dependent effect is isotope fractionation, which occurs in physical processes such as evaporation of a liquid and in chemical reactions. During the evaporation of water, which normally has a source-dependent deuterium concentration of about 0.015 atom percent of the hydrogen atoms, the liquid becomes slightly enriched in D2 O because of its lower vapor pressure. Isotope fractionation can also occur in a chemical reaction so that the ratio of the atoms of one isotope to that of another in the reactant differs from the ratio in the product. An example is an isotope exchange reaction that reaches equilibrium. When 15 NH3 (g) is equilibrated with 14 NH‡ 4 (aq), the ratio of 14 N=15 N in the gas phase becomes about 1.023 times that in the aqueous phase. Another source of isotope fractionation is the kinetic isotope effect that occurs because the rate of a chemical reaction is affected by the mass of the reacting atoms in the reactant. Heavier isotopes form stronger bonds of a given type than lighter isotopes. Thus, the rate of a chemical reaction that involves the breaking of C-H or C-D bonds in isotopomers will be faster for the one with the C-H bonds. The kinetic isotope effect accounts for the enrichment of 12 C relative to 13 C in organic compounds formed in plants by photosynthesis. As we shall see in Chapter 14, Sections 14.5.1, 14.5.2, and 14.5.4., isotope fractionation and its temperature coef®cient have been used to study the mechanisms of a wide variety of biological, chemical, and physical processes in the environment, especially in the paleoenvironment.

13.2.2.2 Nuclear Spin

Using hydrogen as an example, we ®nd that the total nuclear spin associated with an atom of hydrogen in any molecule such as benzene (C6 H6 ) is that of a proton and is equal to 1=2. If we assume that the proton can be treated as a

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

489

rotating charge, it will generate a magnetic ®eld and have a magnetic moment that can interact with an external magnetic ®eld. Thus, when a sample of a hydrogen-containing compound is placed in a strong, homogeneous, external magnetic ®eld, the magnetic moment of the protons becomes oriented in one or the other of two allowed directions corresponding to two magnetic energy states. The energy difference between the two states is proportional to the strength of the external magnetic ®eld and is the order of 10 26 J. If the sample is also irradiated with a pulse of radiofrequency (rf) radiation having energy equal to the energy difference, the sample will absorb the radiation, reduce the intensity of the radiation reaching a detector, and provide a signal that generates a nuclear magnetic resonance (NMR) spectrum. An NMR spectrum can be obtained by varying the rf energy for a ®xed external magnetic ®eld or by varying the magnetic ®eld for a ®xed rf pulse. The electrons in the atoms of a molecule containing hydrogen shield the proton or protons from the external ®eld and cause a small but measurable shift (chemical shift) of the NMR lines. As a result, the NMR spectrum of protons in benzene (C6 H6 ), for example, is shifted relative to that for protons in ethanol (CH3 CH2 OH), because of the different electronic environment of the protons. Furthermore, there are three different electronic environments for protons in ethanolÐone for CH3, one for CH2, and one for OH. NMR spectroscopy provides information about the electronic environment within a molecule and is widely used to determine molecular structure and to study chemical bonding and chemical reactions. Other stable nuclides with I ˆ 1=2 that are used in NMR studies are 13 C, 15 N, 19 F, and 31 P. This very simpli®ed and condensed introduction to NMR is intended to help in the understanding of an important application of stable nuclides and NMR in which the sample of interest is biological tissue and the purpose is to provide information for medical diagnosis. The application is discussed in Chapter 14, Section 14.6.1.1.

13.3 ENERGETICS OF NUCLEAR REACTIONS Mass M and energy E are related through the Einstein equation E ˆ Mc2

…13-1†

where c is the speed of light. The energy equivalent of a change in mass, DM, of 1 amu in a nuclear process corresponds to 149.2 pJ or 931.5 MeV.6

6

The electron-volt (eV) was introduced as a unit of energy in Chapter 4, Section 4.1. One MeV is equal to 106 eV.

490

13.3 ENERGETICS OF NUCLEAR REACTIONS

It is instructive to compare the energy changes in chemical reactions with those in nuclear reactions. For the combustion reaction CH4 …g† ‡ 2O2 …g† ! CO2 …g† ‡ 2H2 O…l†

…13-2†

the standard change in enthalpy at 258C is 890:8 kJ per mole of methane. The reaction is exothermic; that is, heat is given off to the surroundings. For comparison, the energy released when a 23 Na nucleus captures a neutron in the nuclear reaction7 23

Na ‡ 1 n !24 Na ‡ g

…13-3†

8

is 6:71  108 kJ=mol. In this exoergic reaction, which can be written in short notation as 23 Na…n, g†24 Na,9 a nucleus of the only stable isotope of sodium captures a neutron having negligible kinetic energy (about 0.03 eV per neutron or about 2.9 kJ=mol) to become a nucleus of 24 Na. The reaction energy is transferred to the surroundings as electromagnetic radiation (g radiation) and to a relatively small extent as recoil energy (kinetic energy, heat) of the 24 Na atom. On a per-event basis, reaction (13-3) is exoergic by 6.96 MeV per nucleus of 23 Na, and reaction (13-2) is exothermic by 9.23 eV (0.00000923 MeV) per molecule of CH4 . It is not customary to express the energy for nuclear reaction in the units of kilojoules per mole of a reactant or product; it was done here for comparison only. The energy for a nuclear reaction is given for a single event rather than for a mole of events, and for most of the nuclear reactions of interest in this text, the convenient unit of energy is the MeV. Reaction (13-3) will serve to illustrate the calculation of the energy change (Q value) for a nuclear reaction. The equation is rewritten as follows: 23

Na ‡ 1 n !24 Na ‡ g ‡ Q

…13-4†

where Q is introduced to indicate that total energy (rest mass plus any energy transferred into or out of the system) is conserved. Thus, if a nuclear reaction is exoergic, the rest mass of the system decreases by the amount Q, which is transferred to the surroundings as radiation energy and=or kinetic energy. Then, Q is positive. If a reaction is endoergic, the rest mass of the system will increase and Q will be negative by the amount that must be brought into 7 The equation for a nuclear reaction is balanced with respect to reactants and products by conserving mass number and total charge (nuclear and electronic). For the neutron, Z ˆ 0, A ˆ 1; for the proton, Z ˆ 1, A ˆ 1; and for the photon, Z ˆ 0, A ˆ 0. 8 The terms ``exoergic'' and ``endoergic'' correspond to ``exothermic'' and ``endothermic'', but they include all forms of energy, not just thermal energy. 9 The short notation represents the following: target nuclide(particle in, particle out)product nuclide.

491

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

the system (added in some form of energy to the left side of the equation) just to conserve energy.10 Then, for a nuclear reaction, Q ˆ Mreact and for reaction (13-4) we write

 Q ˆ ‰M 23 Na ‡ M 1 n Š

Mprod

‰M

Q ˆ ‰22:989767 ‡ 1:008665Š


24

 Na ‡ M…g†Š

…13-5†

…13-6†

‰23:990961 ‡ 0Š

Q ˆ 0:007471 amu ˆ 6:96 Mev
For the combustion  reaction (13-2), the decrease in mass is only 9:23 eV= 931:5  106 eV=amu ˆ 0:00000000991 amu per molecule or 9:91  10 9 grams per mole of CH4 burned. Therefore, mass change is not a useful measure of the energy absorbed or evolved in a chemical reaction. An example of an endoergic nuclear reaction is the production of 22 Na from stable 19 F by the reaction 19

F ‡ 4 He !22 Na ‡ 1n ‡ Q

…13-7†

For this reaction Q is 0:002096 amu (1.95 MeV). Based on Q, the 4 He, as He2‡ , must be given a kinetic energy equal to 1.95 MeV in a particle accelerator to conserve energy. Since, however, linear momentum must also be conserved in a nuclear reaction, additional kinetic energy must be given to the 4 He to provide kinetic energy for the reaction products. The threshold energy, Ethreshold , (minimum for the reaction to occur) based on only the two conservation laws becomes11

   M 19 F ‡ m 4 He 19 ‡ 4  Q Q …13-8† 19 M…19 F†

4

Ethreshold ˆ 1:95  23=19 ˆ 2:36 MeV Reaction (13-7) was chosen because it introduces another aspect of the energetics of nuclear reactions that must be evaluated whenever a charged particle is a reactant or a product. In this reaction there is an increase in the Coulomb (electrostatic) potential energy (increase in repulsion energy) as the particle with a nuclear charge of ‡4 approaches a target nuclide having a nuclear charge of ‡9. The dependence of the Coulomb potential energy V, in

10

In this traditional way of calculating Q, the difference calculation is in the reverse order of that used to calculate the change in a thermodynamic property (products reactants) for a chemical reaction. The calculation of Q using the chemical convention for nuclear reactions also will be
found in the literature.
 11 m 4 He is the motion mass of 4 He. Both m 4 He and the rest masses are approximated by mass numbers.

492

13.3 ENERGETICS OF NUCLEAR REACTIONS

joules (J), on the magnitude of two electric charges q1 and q2 (in coulombs, C) and the distance of separation r (in meters) is given by Vˆ

1 q1 q2 4pe0 r

…13-9†

In this equation e0 is the permittivity of a vacuum and is equal to 8:854  10 12 J 1 C2 m 1 . The quantity of interest in a nuclear reaction is V 0 , the height of the Coulomb barrier in MeV, that is, the work required to bring the nucleus of the projectile species into contact with the target nucleus. Equation (13-9) becomes V0 ˆ

1:44Z1 Z2 …MeV† R1 ‡ R2

…13-10†

where the charges are Z1 and Z2 and r is replaced by the sum of the nuclear radii of the two reactants, R1 and R2 . The radius of a nucleus in femtometers (10 15 m) is given by R ˆ 1:4A1=3.12 For reaction (13-7), the Coulomb barrier height is 4.35 MeV. When conservation of momentum is taken into account, the new threshold energy is 5.27 MeV. Finally, it is necessary to point out that reaction (13-7) may occur for an incoming 4 He2‡ particle having a kinetic energy less than 5.27 MeV, but not less than 2.36 Mev. The value of 4.35 MeV for the Coulomb barrier height was calculated by means of classical mechanics [equation (13-10)]. When a nuclear reaction is examined in terms of quantum mechanics, an incoming charged particle with kinetic energy less than the Coulomb barrier height has a ®nite probability of penetrating (tunneling through) the barrier. This probability increases with increasing kinetic energy of the particle. If an endoergic nuclear reaction involves a charged particle as a reactant or a product, any excess kinetic energy above Q that is given to the incoming particle because of the Coulomb barrier is distributed among the products. For an exoergic reaction with a Coulomb barrier, the energy available to the products is the sum of the kinetic energy of the incoming particle and the Q value. Another type of energy associated with an atomic nucleus is the binding energy of its nucleons, which is usually expressed as the average binding energy per nucleon. The total binding energy is the energy required for the hypothetical reaction of pulling apart a nucleus into its constituent nucleons. Binding energy is, therefore, a measure of the stability of a nucleus. As an example, the total binding energy of a 23 Na nucleus is the Q value based on the conservation of energy for the following hypothetical reaction: 23

Na ! 111 H ‡ 121 n ‡ Q

…13-11†

12 When the particle in or out in a nuclear reaction is a proton, its radius is usually taken as zero except when the target or product nuclide has a very small mass number.

493

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

Then, Q ˆ ‰M


23

Q ˆ 22:989769 Qˆ

 Na Š


 ‰11M 1 H


 12M 1 n Š

…13-12†

‰…11  1:007825† ‡ …12  1:008665†Š

0:200288 amu ˆ

186:57 MeV

and the average binding energy per nucleon is 8.11 MeV. Figure 13-2 illustrates the way average binding energy per nucleon varies with mass number for stable nuclides. The peak at 7 MeV is for 4 He. The maximum stability is found for elements of mid-range atomic number. A ``rule of thumb'' is to use a value in the range 8±8.5 MeV for the approximate average binding energy per nucleon for stable nuclides of elements between oxygen and tantalum, inclusive. When a radionuclide decays into another nuclide, which may be stable or radioactive, there is a spontaneous decrease in the rest mass of the system. We discuss the energetics of radioactive decay in Section 13.5.

9

Average binding energy per nucleon (MeV)

8 7 6 5 4 3 2 1 0 0

50

100

150

200

Mass number FIGURE 13-2 Dependence of the average binding energy per nucleon on mass number of a nuclide.

494

13.4 THE KINETICS OF NUCLEAR REACTIONS

13.4 THE KINETICS OF NUCLEAR REACTIONS 13.4.1 Radioactive Decay In the simplest case of radioactive decay, radionuclide A is transformed irreversibly (spontaneously) into a stable product B(s) according to an equation such as A  B…s†.13 The probability that the nucleus of a given atom of a radionuclide will decay does not depend on the age of the atom. Furthermore, characteristic of a ®rst-order process, it is not necessary that such a nucleus interact with any other nuclei in a sample containing a large number nuclei in order to undergo radioactive decay. In a ®rst-order process, the number of nuclei decaying per unit time at a given time in a sample containing a large number of a atoms of a given radionuclide is proportional to
, the number of such atoms present at that time. In other words, the fraction of radioactive nuclei decaying per unit time is a constant (l). The differential rate equation for the process has the same form as that for a ®rst-order chemical reaction dN ˆ dt

lN

…13-13†

where N is used instead of concentration, l is the traditional symbol for the rate constant (``decay constant,'' usually in reciprocal seconds), and the negative sign indicates that the number of radioactive atoms in the sample decreases with time. Some radionuclides decay by branching, a more complex process in which decay may occur along two or more paths to give different products. The fraction of nuclei that decays by each mode is a characteristic property of the radionuclide that must be determined experimentally. Since the value of l for a mode of decay is a measure of the probability of decay by that mode, the decay constant for the total rate of decay, loverall , is the sum of the l values for each branch. The disintegration rate lN of a radionuclide in a sample is the radioactivity or ``activity'' A of the radionuclide.14 It is a measure of the amount of the radionuclide in a sample. The curie (Ci) was the accepted unit of radioactivity until 1975, when the new SI quantity of activity, the becquerel (Bq), was introduced.15 The curie was originally equated to the number of disintegrations per second (dps) that occur in a ®xed amount of 226 Ra. It is now de®ned 13

When used to characterize a nuclide, (s) means ``stable.'' By now the reader will have noted that two meanings have been assigned to N and three to A. Fortunately, this rather common practice should not create a serious problem because the intended meaning should be clear from the context in each case. 15 In the late 1940s another unit, the rutherford (rd) was used in some publications. One rd was de®ned as 1  106 disintegrations per second. 14

495

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

as 3:700  1010 dps for any radionuclide. One Bq is equal to 1 dps for any radionuclide (see Table 13-1). Another quantity that is often used, the speci®c activity, is the activity (in becquerels or curies) of a speci®ed radionuclide per unit quantity of radioactive material (e.g., per millimole of a compound or per unit weight of an element). When the differential rate equation (13-13) is integrated between the limits of t ˆ 0 (the beginning of the time period of interest when the sample contains N 0 atoms of a radionuclide) and lapsed time t ˆ t (when the sample contains N atoms), the equation for the number of atoms remaining in the sample becomes N ˆ N 0 exp… lt†

…13-14†

In terms of natural logarithms,
 ln N=N 0 ˆ

lt

…13-15†

lt 2:303

…13-16†

and, in terms of common logarithms,


 log N=N 0 ˆ

After a sample has decayed so that N=N 0 ˆ 1= 2, the lapsed time is the half-life t1=2 of the radionuclide. Then,
 ln N=N 0 ˆ ln0:5 ˆ lt1=2 ˆ 0:693 …13-17† and the decay constant is related to the half-life by the equation lˆ

0:693 t1=2

…13-18†

TABLE 13-1 Units of Radioactivity Curies 1 pCi 27.0 pCi 1 nCi 1 mCi 1 mCi 1 Ci 1 kCi 1 MCi 1 GCi

Disintegrations per second (dps) 3:70  10 2 1 37 3:70  104 3:70  107 3:70  1010 3:70  1013 3:70  1016 3:70  1019

Becquerels 37 mBq 1 Bq 37 Bq 37 kBq 37 MBq 37 GBq 37 TBq 37 PBq 37 EBq

496

13.4 THE KINETICS OF NUCLEAR REACTIONS

Because it is the half-life of a radionuclide that is given in nuclear data tables,16 it is more convenient to express equation (13-14) in terms of t1=2 . Thus we write   0:693t …13-19† N ˆ N 0 exp ˆ N 0 …1= 2†t=t1=2 t1=2 In certain calculations the mean life  is used. It is equal to 1=l and 1:443t1=2 . For most purposes it is the change of the activity of a sample of radioactive material with time that is of interest rather than a change in the number of radioactive atoms. After multiplication of equation (13-14) by l and replacement of lN and lN 0 by A and A0 , the equation for time dependence of activity becomes A ˆ A0 exp… lt†

…13-20†

A typical semilog plot of the activity of a single radionuclide with a half-life of 2.0 days is shown in Figure 13-3 (A0 ˆ 800 Bq). When the rate at which radiation is emitted by a radioactive source is measured in the laboratory or in the ®eld, the observed counting rate R is proportional to the activity. If the proportionality factor does not drift during a series of measurements, the counting rate (e.g., counts per minute) will have the same time dependence as A. Then R and R0 can be substituted for A and A0 , respectively, in equation (13-20). For a single radionuclide, the decay curve based on counting rates will resemble that in Figure 13-3 except that the data points will scatter about the ``best'' straight line because of statistical ¯uctuation of radioactive decay. Most of the radionuclides that occur in nature and those produced in nuclear power reactors are components of a complex mixture. There are three kinds of mixture: 1. Those containing independent components, each decaying as just described 2. Those containing one series or several series, each having genetically related members (i.e., the ®rst member in a series decays into the second, which decays into the third, etc., as discussed shortly) 3. Those containing a combination of types 1 and 2. 16 In this text, half-lives are given in parentheses after the symbol for the radionuclide. The units are seconds (s), minutes (m), hours (h), days (d) and years (y). In some data compilations ``a'' is used for years. Nuclidic data in Chapters 13 and 14 were taken from Parrington et al. Chart of the Nuclides and the CRC Handbook of Chemistry listed at the end of the chapter under Additional Reading and Sources of Information.

497

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

Activity (Bq)

1000

t1/2

100

2t1/2

10

0

2

4

6

8

10

Time (days)

FIGURE 13-3 Semi log plot of the decay curve for a radionuclide with a half-life of 2.0 days and A0 ˆ 800 Bq.

A semilog plot of the decay curve for the total activity of a type 1 mixture will be concave upward corresponding to the sum of the straight-line decay curves for the activities of the components. An example is shown in Figure 13-4 for a mixture of two independent components, A and B, whose half-lives are 10.0 and 1.0 h, respectively, and A0 ˆ 200 Bq, B0 ˆ 600 Bq. An example of the decay sequence for a type 2 mixture consisting of a chain with three radioactive members (without branching) and a stable end product is illustrated by lA

lB

lC

A ! B ! C ! D…s†

…13-21†

where radionuclide A is the parent of daughter B, which becomes the parent of C, which decays to the stable nuclide D. The rate of decrease of the number of atoms of A [in reaction (13-21) ] is independent of the radioactivity of the daughters and is given by the differential rate equation (13-13) with N changed to NA and l to lA . For atoms of daughter B, however, the total rate of change is equal to the rate of their formation by decay of A, the parent, minus the rate of their decay, so that the differential equation is

498

13.4 THE KINETICS OF NUCLEAR REACTIONS

1000

A+B 100

Activity (Bq)

A B

10

1

0.1 0

5

10

15

20

Time (h)

FIGURE 13-4 Semi log plot of the decay curves of the total activity and the activities of the two independent components, A (10.0 h, A0A ˆ 200 Bq) and B (1.0 h, A0B ˆ 600 Bq) in a mixture.

dNB ˆ lA N A dt

lB N B

…13-22†

This equation is for the simplest case, in which the only removal process for nuclide B is radioactive decay. Other processes that can remove B include chemical separation, loss by volatilization, and conversion into another nuclide by nuclear reaction in an accelerator or nuclear reactor. After equation (13-22) has been integrated and the number of atoms changed to activity, the following equation is obtained: AB ˆ A0A

lB lB

lA

‰exp… lA t†

exp… lB t†Š ‡ A0B exp… lB t†

…13-23†

where the last term accounts for the decay of any B that is present in the sample at time t ˆ 0. General expressions (e.g., the Bateman equation),17 are available for the equation obtained by integration of an equation like equation (13-22) for the nth member of a series. 17

H. Bateman, Solution of a system of differential equations occurring in the theory of radioactive transformations, Proc. Cambridge Philos. Soc., 15, 423 (1910).

499

13. ATOMIC NUCLEI, RADIOACTIVITY, AND IONIZING RADIATION

There are three naturally occurring, radioactive series, namely, the uranium, the thorium, and the actinium series. Each series is named after the longestlived and, therefore, ®rst member. The transitions that occur in the uranium series are represented in Figure 13-5. Data and names used in the older literature for the members of the uranium series are given in Table 13-2. Similar information for the thorium and actinium series is given in Appendix B. The uranium series is also known as the 4n ‡ 2 series because the mass number of each member can be expressed as (4n ‡ 2), where n is an integer. Similar designations for the thorium series and the actinium series are 4n and 4n ‡ 3, respectively. The three series contain examples of branching, already mentioned, and the three types of parent±daughter system described next.

92 (U)

234 m

91 (Pa) 90 (Th)

234

238

234

234 230 –

89 (Ac) 88 (Ra)

226

87 (Fr) 86 (Rn)

222 218

85 (At) 84 (Po) 83 (Bi) 82 (Pb) 81 (Tl) 80 (Hg)

210

214

218

210

214 210

214

206 (s) 206

210 206

FIGURE 13-5 Uranium (4n ‡ 2) series. The main sequence is indicated by arrows and a dash.

500

13.4 THE KINETICS OF NUCLEAR REACTIONS

TABLE 13-2 Uranium (4n ‡ 2) Series Nuclidea

Half-life

92 92 91

U (UI) U (UII) 234m Pa (UX2 )

4:47  109 y 2:46  105 y 1.17 m

91 90 90 88 86 85 84

234

Pa (UZ) Th (UX1 ) 230 Th (Io) 226 Ra (Ra) 222 Rn (Rn) 218 At 218 Po (RaA)

6.69 h 24.10 d 7:54  104 y 1599 y 3.8235 d 1.5 s 3.10 m

84 84 83

214

Po (RaC0 ) Po (RaF) 214 Bi (RaC)

163:7 s 138.38 d 19.9 m

83

210

Bi (RaE)

82 82

214 210

Pb (RaB) Pb (RaD)

Z

82 81 81 80

238

234

234

210

206

5.01 d 27 m 22.6 y

Pb (RaG) Tl (RaC 00 ) 206 Tl (RaE00 ) 206 Hg 210

Stable 1.30 m 4.20 m 8.2 m

Radiationb   IT, 0.13% b , 99.87% b ,g b , …g† a a, …g† a a a, 99.98% b , 0.02% a a a, 0.02% b , 99.98%, g a, 1:3  10 4 % b , 99‡ % b ,g a, 1:7  10 6 % b , 99‡ %, (g) b ,g b b ,g

a

Symbol used in the early studies of naturally occurring radioactivity is given in parentheses [(Io) ˆ ionium]. b (g) indicates low intensity (1±5%); g rays with intensity below 1% are not included. Where (IT and b ) or (a and b ) is given, branched decay occurs.

If nuclide A in equation (13-21) has a very long t1=2 relative to that of B, corresponding to lA 13  1013 105  1011 238  1015 106  1011 7  1015 11  1014 20  1015 378  1010 > 12  1015 2  1015 43  1010 65  1011 140  1010 704  108 447  109 80  107

EC, b EC b b b EC EC, b a a a a a b EC, b a b a a a a a

Detectable.

potassium [0.0117 at. % 40 K …127  109 y† ]. The concentrations are generally less in basic igneous rocks, sedimentary rocks, and limestones. Based on the average concentrations in the crust, the ratio of Th to U is about 4. Uranium in rocks and soils consists of three long-lived isotopes: 238 U (99.274%) (447  109 y), parent of the uranium series; 235 U (0.720%) (704  108 y), parent of the actinium series; and 234 U (0.0055%) (246  105 y), a member of the uranium series. In normal soil the radioactivity of 238 U is about 20 Bq=kg (0.54 nCi=kg) and that for 40 K about 400 Bq=kg (11 nCi=kg). In rocks, soils, and sands containing the thorium series, the isotopes of thorium present are 232 Th (140  1010 y) and a daughter, 228 Th (1.913 y). The 238 Th activity in soils is about 40 Bq=kg (about 1 nCi=kg). If uranium is also present, the thorium isotopes will include those in the uranium series and the actinium series. The g-emitting members of the three series (Figure 13-5, Table 13-2, and Appendix B) and 40 K account for the above-normal radiation background often associated with granitic rock. In undisturbed rock, all the members of a given

14. THE NUCLEAR ENVIRONMENT

567

series are present in secular equilibrium and, therefore, have the same disintegration rate. However, each series contains a radioisotope of the inert gas radon, which can escape into the atmosphere to a limited extent from porous rock or rock with cracks but can escape much more readily from permeable soils. Usually the radon escapes into the atmosphere from the top meter or two of soil. In a given series, the members that follow the radon isotope have less than the equilibrium disintegration rate in rock or soil from which radon has escaped. Of the three radon isotopes 219 Rn (3.96 s), 220 Rn (55.6 s), and 222 Rn (3.8235 d) that can escape into the atmosphere, 222 Rn in the uranium series has been linked to lung cancer and is the most important environmental contaminant. Its concentration in soil ranges from a few hundred becquerels per cubic meter to over 37 MBq=m3 (tens of picocuries per liter to over 100 nCi=liter). Its nonvolatile parent, 226 Ra (1599 y), has a speci®c activity of 37±74 Bq=kg (1±2 pCi=g) in soil.5 Most coal used by power plants in the United States has a uranium concentration of 1±4 ppm and about the same range for thorium. When coal is compared with common rocks, the concentration is about the same for uranium but is lower for thorium. Eastern U.S. coal contains about 18 Bq=kg (0.5 pCi=g) of 226 Ra. The concentration in British coal is in the range of 1.8±11 Bq=kg (0.05±0.3 pCi=g). When coal is burned, the 222 Rn enters the atmosphere and its parent (226 Ra) remains in the ash, where its concentration is increased by a factor of perhaps 10 over that in the coal, depending on the composition of the coal.

14.4.2 Uranium and Thorium Ores There are over 100 minerals that contain uranium. Only a few of these are found in deposits that are economically signi®cant. The uranium content of an ore is expressed as a percentage of U3 O8 and is commonly in the range of 0.1±0.5%, although ores with much higher uranium content have been found. Examples of speci®c ores are uraninite, which varies in composition from UO2 to UO2
2UO3 or U3 O8 (known as pitchblende), and carnotite (K2 O
2UO3
V2 O5
xH2 O), which, in the past (before 1943), was mined in the United States mainly for its vanadium content. Commercial-grade uranium ores have also been mined in Australia, Canada, China, France, Gabon, Germany, Namibia, Portugal, Russia, South Africa, and the United Kingdom. Thorium, like uranium, is widely distributed on the earth and is commonly found associated with uranium, but the concentrations of thorium in uranium ores are generally not high enough to be commercially interesting. The principal source of thorium is monazite, (Ce, La, Y, Th) PO4 , which occurs as beach and 5

The density of soil is typically in the range of 1600±2600 kg=m3 .

568

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

river sands produced by the weathering of rocks. Signi®cant sources of monazite occur in Australia, Brazil, China, India, South Africa, and the United States (Colorado, Florida, Idaho, Montana, North Carolina, and South Carolina). In the past, monazite was mainly of interest as a source of rare earths and ThO2 , which was used in gas mantles. The thorium content of monazite is usually in the range of 1±10% ThO2 .

14.4.3 The Atmosphere 14.4.3.1 Outdoor Air

The natural radioactive contaminants of the atmosphere are 222 Rn, its progeny, and, to a much lesser extent, the cosmogenic 3 H and 14 C. As far as is known, the latter two radionuclides have always been present in the atmosphere, but their rates of formation have not been constant over long periods of time (tens of thousands of years) owing to variations in the intensity of cosmic radiation, especially that of solar origin. Long-term changes in the 14 C=12 C ratio in the atmosphere resulting from changes in the earth's magnetic ®eld are shown in Figure 14-1. Short-term variations are assumed to arise from variations in the solar component of cosmic radiation. During the past hundred years, the 14 C:12 C ratio in the atmosphere has changed for two additional reasons. First, with the beginning of the industrial era at the end of the nineteenth century, the combustion of fossil fuels (high in 12 C, low in 14 C) led to a decrease in the ratio (the Suess effect). Second, beginning

Change in 14C (%)

10

5

0

BC/AD −5

7000

6000

5000

4000 3000 2000 1000 Years of tree ring growth

0

1000

2000

FIGURE 14-1 Long-term variation in atmospheric 14 C activity as determined from tree rings. Adapted from G. Choppin, J. O. Liljenzin, and J. Rydberg, Radio-chemistry and Nuclear Chemistry, 2nd ed. Copyright # 1995. Reprinted by permission of Butterworth-Heinemann, Oxford.

569

14. THE NUCLEAR ENVIRONMENT

with the atmospheric testing of nuclear weapons in 1954, there was an increase in 14 C (5715 y) concentration caused by the 14 N…n, p† 14 C reaction [reaction (14-2) ], with neutrons released in atmospheric testing of nuclear weapons, especially ``H-bombs.'' (Section 14.11.1). Before testing, the 14 C content of plants and animals was 022 Bq=g of carbon (6 pCi=g). By the time atmospheric testing of nuclear weapons ended in 1963, the concentration of 14 C had risen to about double the natural value, as shown in Figure 14-2. Tritium (12.32 y) in the atmosphere is present as HTO and is in equilibrium with HTO in water on the earth that is in contact with the atmosphere. Prior to 1954, the tritium content of the biosphere was estimated to be about 900 g or about 0.33 EBq (about 9 MCi). Its concentration is sometimes expressed relative to 1 H in tritium units, where 1 TU ˆ 1 3 H atom per 1018 atoms of 1 H. For water, 1 TU is 122 Bq=m3 (33 pCi=liter). The level of 3 H in rainwater increased from the range of about 0.5 to 5.0 T U before 1954 to values as high as 500 T U after the testing of tritium-containing thermonuclear weapons. From the effects of weapons testing on 3 H concentration, the residence time of 3 H in the stratosphere has been estimated to be 2±4 years. Tritium is washed from the troposphere in about 2 months.

100 90

Percent above normal

80 70 60 50 40 30

Northern Hemisphere

20 10

Southern Hemisphere

0 1956 1957 1958 1959 1960 1961 1962 1963 1964 1965

FIGURE 14-2 Increase in tropspheric 14 C from atmospheric testing of nuclear weapons. Normal air was taken to contain 74  105 atoms of 14 C per gram of air in 1954. Adapted from Report of the United Nations Scienti®c Committee on the Effects of Atomic Radiation (UNSCEAR), Supplement No. 14 (A=6314). United Nations, New York. Copyright # 1966. Used by permission of the United Nations.

570

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

Radon, predominantly 222 Rn (3.8235 d) in the uranium series, is present everywhere in the earth's atmosphere because it is a descendent of 238 U, and uranium is an ubiquitous element. Although the main source of radon in the atmosphere is radon in soil, radon dissolved in spring water or well water that has been in contact with rocks or soil or sediments containing uranium also escapes when the water is exposed to the atmosphere. At any one location the concentration of radon in the atmosphere varies diurnally and seasonally and changes rapidly with atmospheric conditions. A typical value for 222 Rn in the United States is about 56 Bq=m3 (015 pCi=liter). Worldwide concentrations have been reported to be from 4±18 Bq=m3 (01 05 pCi=liter). For 220 Rn (55.6 s), a member of the thorium series, the value is about 07 Bq=m3 (002 pCi=liter). If decay products formed in very small amounts by branching are neglected, the important progeny of 222 Rn are given in the following equation: 222 214

a

Po !

a

Rn !

210

b

218

Pb !

a

Po !

210

b

214

Bi !

b

Pb !

210

a

214

Po !

b

Bi !

206

…14-3†

Pb …s†

All are radioisotopes of nonvolatile elements, and except for 210 Pb (22.6 y) and Po (138.38 d) they are short-lived. (See Figure 13-5 and Table 13-2.)

210

14.4.3.2 Radon in the Air in Mines and Buildings

When it was observed in the 1920s that uranium miners suffered from a relatively high incidence of lung cancer, the trend was at ®rst attributed to radon in the air in the mines. Later it was shown that the effect is caused not by radon itself, but by its two short-lived a-emitting daughters, 218 Po (3.10 m) and 214 Po (163.7 ms).6 Thus, radon is really the carrier for its nonvolatile progeny, and because of its half-life of almost 4 days it can, once airborne, travel a considerable distance from its point of origin. If the progeny are formed in air, a fraction becomes attached to aerosols (e.g., tiny droplets of water, dust, tobacco smoke, etc.), and the remainder remains unattached. As an inert gas, inhaled radon is readily exhaled. On the other hand, when the short-lived radon progeny are inhaled, they deposit in the lungs, where they remain and emit a particles that are absorbed in lung tissue. In 1956 a unit of radioactivity, the working level (WL), was introduced in connection with the establishment of acceptable levels of radon daughters for the air in mines.7 One WL, a unit of exposure, is associated with any combin6 While airborne, the long-lived 210 Pb and 210 Po are not considered to contribute signi®cantly to lung cancer. They are of interest, however, because they are washed out of the atmosphere by rain onto tobacco and other vegetation, where they become concentrated. 7 The radon daughter hazard in underground mines is not limited to uranium mines, because uranium is a constituent of many rocks and ores.

14. THE NUCLEAR ENVIRONMENT

571

ation of the short-lived radon daughters in one liter of air at ambient temperature that results in the ultimate release of 13  105 MeV of a-particle energy. One WL is, then, approximately equal to the a energy emitted per unit volume of air by the short-lived progeny in equilibrium with 37 kBq=m3 (100 pCi=liter) of 222 Rn. A related cumulative exposure unit, the workinglevel month (WLM), is de®ned for miners as the number of working levels of exposure in one working month (170 hours). One WLM is equal to 35  10 3 J=h per cubic meter of air. On the average, a miner with an exposure of 1 WLM receives a dose of about 8 mGy (0.8 rad). In 1961 almost 30% of the underground uranium mines in the United States had WLs greater than 10. Six years later, after improvements had been made in ventilation, only 1% of the mines had a WL exceeding 10. Although a working-level month is de®ned as 170 hours, an actual month is 720 hours (30 days). Thus, for a person occupying a house for 16 hours a day for one actual month of 30 days at 1 WL, the cumulative exposure would be 2.82 WLM. The dose received by the average person for an exposure of 1 WLM would be about 4.5 mGy (0.45 rad). Radon has been present in the air in our homes ever since people began living in caves, and there is extensive literature on both the sources and the health effects of radon. In recent years there have been numerous documented cases of elevated radon levels in houses and other buildings. The following are examples  In 1983 it was discovered that radon levels were elevated in several houses in Glen Ridge, Montclair, and West Orange, New Jersey, because the soil used as ®ll around the basements and in the yards was contaminated with 226 Ra, radon's parent. Presumably, the soil came from a site where there had been a plant in which 226 Ra was separated from uranium ore. Some of the residents had to leave their homes temporarily. The contaminated soil was removed, packaged in drums, and stored on the site until, after several years, it was transported to a disposal site for low-level radioactive waste.  In 1986 about 100 homes in Clinton, New Jersey, were found to have high radon levels [some > 37 kBq=m3 (1000 pCi=liter)]. The homes were built on a cliff near an old quarry that contained limestone with an atypically high concentration of uranium. Remedial procedures described shortly were used to reduce the radon levels.  Elevated radon concentrations have been found in the air in buildings in California located over shale that releases radon and in buildings whose construction involved the use of tailings from nearby uranium mines (e.g., in Colorado) and residues from phosphate mines (e.g., in Florida) (see Section 14.4.6). The ``radon hazard'' in the home suddenly received nationwide attention early in 1985. In December 1984 an engineer who worked at a nuclear power

572

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

plant in Boyertown, Pennsylvania, set off the alarm on a radiation monitor one day when he entered the plant. Such monitors are used to detect contaminated clothing on workers leaving a facility where radioactive material is used. In this incident, the person's clothing was contaminated with radon progeny present in the air in his house, where the radon level was found to be above 93 kBq=m3 (> 25 nCi=liter). In terms of the hazard of ionizing radiation, it was safer to be at work in a nuclear power plant than to be at home. The area where this event occurred is known as the Reading Prong (Figure 14-3), a geological formation that extends northeasterly from Reading, Pennsylvania, to the western edge of Connecticut. Radon levels found in some of the houses in the region are among the highest in the United States. In 1985 the U.S. Environmental Protection Agency established a nationwide program to assist states and homeowners in reducing the risk of lung cancer from indoor radon. In the following year, EPA recommended that remedial action be taken if the radon level in a home exceeded 0.025 WL or 148 Bq=m3

0

10

20

30

CONN.

Miles

Peekskill

NEW YORK Suffern

N

New York City

READING PRONG Morristown Phillipsburg

PENNSYLVANIA Riv er

Boyertown

Trenton

Reading De la

Philadelphia

MD. DEL.

e ar w

NEW JERSEY Atl a Oc ntic ean

Easton Allentown

FIGURE 14-3 Uranium-rich Reading Prong. Redrawn from ``Radiactive Gas Alters Lives of Pennsylvanians,'' by William R. Greer. The New York Times, October 28, 1985. p. A10. Used by permission of The New York Times.

573

14. THE NUCLEAR ENVIRONMENT

Geologic Radon Potential (predicted average screening measurement)

Low (4 pCi/liter) Scale Continental Untied States and Hawaii Scale 0

500

Miles

0

Miles

500

FIGURE 14-4 Generalized geologic radon potential of the united states by the U.S. Geological Survey. From EPA's map of radon zones (separate issue for each state), U.S. Environmental Protection Agency Document 402-R-93-052, 1993.

(4 pCi=liter).8 In 1993 EPA issued reports containing maps of ``radon zones'' for each state. The reports contained two maps (Figures 14-4 and 14-5) of the continental United States and Hawaii. Figure 14-4, originally prepared by the U.S. Geological Survey, identi®es regions where the predicted indoor radon potential is low, moderate, or high. Figure 14-5 shows three predicted zones of radon concentration in the air in the lowest livable area of a building: greater than 4 pCi=liter, equal to or greater than 2 pCi=liter, and less than 2 pCi=liter, for 3141 counties. The indicators used for radon potential included indoor radon measurements, geology, aerial radioactivity, soil parameters, and foundation types. It is very important to realize that the radon concentrations are predicted values and that actual values can differ signi®cantly and unexpectedly.

8

Because this value was obtained by using the linear no-threshold hypothesis and extrapolating from dose±effect data for miners, it has been criticized as being too high.

574

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

Legend Zone 1 Zone 2 Zone 3

Guam – Preliminary Zone designation.

FIGURE 14-5 EPA map of radon zones in the United States: Zone 1, > 148 Bq=m3 … > 4pCi=liter†; Zone 2,  74 Bq=m3 …  2pCi=liter†  148 Bq=m3 …  4pCi=liter†; Zone 3, < 74 Bq=m3 … < 2pCi=liter†. The map is accompanied by the following statement from the EPA: ``This map is not intended to be used to determine if a home in a given zone should be tested for radon. Homes with elevated levels of radon have been found in all zones. All homes should be tested, regardless of geographic location.'' From EPA's map of radon zones (separate issue for each state), U.S. Environmental Protection Agency Document 402-R-93-052, 1993.

A measured value for the concentration of radon in a building depends on the method of measurement used, the season of the year, the climatic conditions, the construction of the building, the type of soil surrounding and below the basement of the building, the source of water (e.g., well or reservoir), and so on.9 As a very approximate guide, if the water used in a home has a radon 9 There are several very different devices available for measuring the radioactivity that can be attributed to radon in the air in a home. Radon data require careful interpretation, and measurements should be made after consultation with the local health department. Radon measurements in a residence should be made at the living level and should be repeated several times. If the basement contains a bedroom or living room, it should be included.

14. THE NUCLEAR ENVIRONMENT

575

concentration of 370 MBq=m3 (10 mCi=liter), it could increase the radon content of the air by about 37 Bq=m3 (1 pCi=liter). In the United States, indoor radon levels of 3.7±7.4 Bq=m3 (1±2 pCi=liter) are ``normal.'' For levels above 148 Bq=m3 (4 pCi=liter), the EPA recommends that follow-up measurements be made to establish a value that can be used to determine whether remedial action should be taken and, if so, how urgent it is to reduce the level to about 148 Bq=m3 (4 pCi=liter) or less.10 For levels between 148 and 740 Bq=m3 (4 and 20 pCi=liter), the EPA recommends reducing the level within a few years; for levels between 740 Bq=m3 and 740 kBq=m3 (20 and 200 pCi=liter), within several months; for levels over 74 kBq=m3 (200 pCi=liter), within several weeks. Estimates of the number of homes in the United States that have radon levels above 148 Bq=m3 (4 pCi=liter) vary from region to region, but the country-wide value at the time of writing is about 6%. The literature contains many publications on radon levels in buildings worldwide. For example, the national mean concentration of radon in indoor air in Finland is 120 Bq=m3 (33 pCi=liter), but values as high as 370 Bq=m3 (10 pCi=liter) have been measured. As another example, Figure 14-6 shows relative radon levels in homes in Great Britain, where the average level is 21 Bq=m3 (054 pCi=liter), but values about 500 times greater have been measured. The two counties with the highest level, Cornwall at the southwestern tip and adjacent Devon, have an estimated 60,000 homes with radon levels above 200 Bq=m3 (54 pCi=liter), the recommended action level. A level of radon high enough to create a health problem in a building can generally be attributed to radon in the soil in contact with the walls and ¯oor of the basement or under the slab in the absence of a basement. As a gas, radon can migrate most easily in coarse, gravelly soil and least easily in clay. It enters a basement by way of crawl spaces, gaps around pipes, cracks in a cement ¯oor or in the basement walls, gaps between the basement ¯oor and the walls, porous cinder blocks, the well of a sump pump, and so on. The maximum concentration of radon can be expected in the basement, with amounts decreasing as one goes to upper ¯oors. Radon migrates to upper ¯oors by way of stairways, gaps, around pipes, and so on. Leakage of radon into a basement can be reduced somewhat by sealing all cracks and openings, but this approach has been shown to have limited bene®t. There are two driving forces for the migration of radon from soil into a basement. One is diffusion from the higher concentraton in the soil to the lower concentration in the basement. The second and more important one, especially for permeable soil, is the pressure gradient that exists when the air 10 The method used to set the value of 4 pCi=liter includes the assumption that there is no safe level; that is, there is not a cutoff value. Thus 3 pCi=liter is not safe. As a practical matter, it may be dif®cult to lower a very high level below 4 pCi=liter.

576

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

FIGURE 14-6 Radon levels in Britain showing the highest readings (> 200Bq=m3 ) in the counties of Cornwall and Devon in southwest England. From Nucl. News, 33, 56 (March 1990). Reproduced from a chart on radiation doses published by the National Radiological Protection Board.

pressure inside is less than that outside a building. It is very easy to create a slightly negative pressure in a house. A heating unit such as a furnace or ®replace that uses fossil fuel will reduce the air pressure as oxygen is removed from the air and vented as CO and CO2 . The heating units themselves, including radiators, and other sources of heat such as a clothes dryer and a kitchen range, cause the air to rise within the house, creating a pressure

14. THE NUCLEAR ENVIRONMENT

577

differential as the house itself behaves like a chimney. Even a strong wind can cause a reduced pressure in a building by the Venturi effect. Ventilation may reduce or increase the radon concentration in a building. Window fans that exhaust air from a building reduce the air pressure in the building, thereby enhancing the ¯ow of radon from the soil into the building. If the radon level is such that remedial action is advisable, the level can be lowered to a value approaching that of the air outside the building by pulling air in from the outside to provide a positive pressure in the building. This also can establish an air¯ow from the upper levels to the basement. When the radon level in a house is very high, a more costly method of lowering the level may be necessary. An effective method is to pull the radonladen air from the layer of gravel or crushed stone under the basement ¯oor and=or outside the basement walls by a fan through piping, whereupon the air is exhausted into the atmosphere above the rooftop. For buildings located where the temperature can drop below freezing, a potential problem is that the cold air pulled under the basement ¯oor can cause moisture condensation and structural damage to the ¯oor. If radon is known to be a potential problem before a house is built, features can be incorporated in the house to minimize the radon level. Thus, it would be expedient to provide a layer of crushed stone or gravel and to install pipes so to permit removal of the radon, and venting to the atmosphere, as just described. The level of the important radon progeny (218 Po and 214 Po) in a building can also be lowered by methods that utilize the properties of the radon progeny. A ceiling fan, for example, will increase the rate at which these attached and unattached positively charged particles reach and become adsorbed by the walls, ceiling, and ¯oor of a room. Because of the charge on the particles, positive ion generators assist in moving the particles toward surfaces of a room. Air cleaners that ®lter or electrostatically precipitate particulate matter in the air remove the progeny, but not the radon and, therefore, leave relatively little dust to which newly formed progeny can become attached. These smaller, unattached particles have the potential of producing a higher dose to the lungs.11 Another way by which the radon level in a home can become elevated is through the use of natural gas in space heaters and unvented kitchen ranges. Radon-222 in the natural gas is released into the air in homes that use such devices. Natural gas used for heating in homes and in industry and for power generation is also a direct source of 222 Rn in the atmosphere. The radon content of natural gas varies from source to source, but the average for most of the United States is about 740 Bq=m3 (20 pCi=liter). Natural gas from gas ®elds in Kansas, Colorado, New Mexico, and the Texas Panhandle may contain higher levels of about 185 kBq=m3 (50 pCi=liter). 11

D. W. Moeller, Nucl. News, pp. 36±39, June 1989.

578

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

Radon-222 from materials used for building construction is discussed in Section 14.4.6. 14.4.4 Water The important naturally occurring radionuclides in water are 226 Ra (1599 y), (a, g) and its a-emitting daughters 222 Rn (3.8235 d), 218 Po (3.10 m), and 214 Po (163.7 ms) in the uranium series and, to a somewhat lesser degree, 228 Ra (5.76 y), (b , low energy, low intensity g) in the thorium series (Appendix B). The 226 Ra content of water in public water supplies varies from being almost undetectably low to as high as about 185 Bq=m3 (5 pCi=liter). Standard water treatment procedures used in municipal water supplies remove most of the 226 Ra. Supplies that depend on wells often have somewhat elevated levels. A typical value for tap water is 15 Bq=m3 (004 pCi=liter). At spas the level in spring water can go to values in excess of 37 kBq=m3 (100 pCi=liter) and ``arti®cial radium waters'' have been used with over 74 MBq=m3 (2.0 mCi= liter). At a given spa having several springs, the radium content can vary widely from spring to spring. Although the existence in the waters of certain spas of 226 Ra, a bone-seeker like Ca, has been known for over six decades, it has been only in recent years that recommendations have been made to limit the daily intake of such waters by individuals. Similarly, hot water and steam that is tapped for geothermal generation of power can have appreciable natural radioactivity. The maximum contaminant level (MCL) of 226 Ra in water for a large population is considered to be 122 Bq=m3 (3.3 pCi=liter). The maximum level set by the EPA for combined 226 Ra and 228 Ra in community water systems is 185 Bq=m3 (5 pCi=liter).12 For gross a particle activity (including 226 Ra, but excluding radon and uranium), the maximum level is 555 Bq=m3 (15 pCi=liter). For uranium, the MCL is 30 mg=liter. The concentration of radon in drinking water obviously depends on the source of the water. In general, as one might expect, the concentration in groundwater, (e.g., well water) can be much higher (e.g., > 104 pCi=liter) than in surface water, where the concentration is negligible. Because the most serious health risk of radon is considered to be lung cancer, radon in drinking water presents a relatively lower risk for lung cancer unless it becomes airborne and contributes signi®cantly to the radon already in the air. However, a study made by the Committee on the Biological Effects of Ionizing Radiation of the NRC (National Research Council) estimated the number of stomach cancers that can be caused by radon progeny in drinking water and compared the number with that for lung cancer. The comparison is shown in Figure 14-7. 12

Code of Federal Regulations, Title 40, Part 141, 15, U.S. Environmental Protection Agency, 2000.

579

14. THE NUCLEAR ENVIRONMENT

Cancer risk due to radon results from inhalation of air and ingestion of water

Inhalation risk Breathing air with radon

Ingestion risk Drinking water with dissolved radon

, cers can ing1 g n k u l o ,000 m sm 160 ly fro n mai

g 2 thin s) brea moker m s fro ong m cers can eaths a g n d u l t 0 os 9,00 r (m ing 1 ed 1 oor ai t a ch uses eath3 d m r a i m n b t i m s o n E fr to all ca om ome on i from 00 s cers h rs fr rad can s3 cers n3 nce in the 14,0 er from g a n c n a r c c lu tdoo do lung ater can ach u g ra 700 160 from w stom ntainin ted adon o d a 0 e t m 2 o ted ma Esti thing r ated ter c Esti n emit stim ing wa o E brea d a k r drin 1American

Cancer Society (1998) VI Report (National Research Council 1999) 3Commission on Life Sciences, Committee on Risk Assessment of Exposure to Radon in Drinking Water, National Research Council, National Academy Press, Washington, DC (1999) 2BEIR

FIGURE 14-7 Comparison of lung and stomach cancer fatalities in the United States in 1998. From Commission on Life Sciences, Committee on Risk Assessment of Exposure to Radon in Drinking Water, Risk Assessment of Radon in Drinking Water, National Research Council, National Academy Press, Washington, DC, 1999.

580

14.4 DISTRIBUTION OF NATURALLY OCCURRING RADIOACTIVITY IN THE ENVIRONMENT

Radon can be removed effectively from water by ®ltering through granular activated charcoal. For water with very high levels of radon, care must be taken to change the charcoal ®lter before the adsorbed g-emitting radionuclides become a radiation hazard. Several times beginning in 1997, the EPA has proposed regulations to limit the amount of radon in public water supplies and in schools and hospitals that use groundwater. At the time of this writing, the proposal was in the ®nal review stage. The main source of natural radioactivity in the ocean is 40 K (127  109 y) (112 kBq=m3 , 30 pCi=liter). The second highest source is 87 Rb (488 1010 y) (11 kBq=m3 , 30 pCi=liter). Secular equilibrium (Section 13.4.1) is not attained for the members of the uranium and thorium series in the ocean because of adsorption by sediment of some of the elements in the series, especially thorium (e.g., 230 Th, in the uranium series). Although the uranium content of seawater is very low (e.g.,  3 ppb), the uranium is extractable; hence, seawater is considered to be a future source of uranium for nuclear power plants. Uranium contained in the oceans represents a reserve of about 5 billion metric tons. Seawater also contains about 1  10 10 g of thorium per liter.

14.4.5 Food The naturally occurring a activity of food is mainly associated with 226 Ra (1599 y) in the uranium series, its a-emitting progeny [especially 210 Po (138.38 d) ], and the a-emitting daughters of 228 Ra (5.76 y) in the thorium series. Both 210 Pb (22.6 y) and its daughter 210 Po can enter food not only from the soil, but also from the atmosphere, where they are present as the daughters of 222 Rn. Examples of atmospheric concentrations at ground level are 148 mBq=m3 (4 aCi=liter) for 210 Pb and 37 mBq=m3 (1 aCi=liter) for 210 Po. For leafy vegetables, the 210 Pb and 210 Po contents are determined more by ``natural fallout and rainout'' from the atmosphere than by the composition of the soil. Food accounts for 80±90% of the intake of 226 Ra, with the remainder coming from water. The average daily intake of 226 Ra is about 110 mBq (3 pCi) in food having 37 370 mBq=kg (1 10 pCi=kg). Cereals and other grain products, vegetables, and fruits are the main sources. Speci®c examples of approximate speci®c activity [in mBq=kg and (pCi=kg) ] are whole-wheat bread 111 (3), milk 9 (0.24), potatoes 56 (1.5), fruit 48 (1.3), fresh vegetables 74 (2), ®sh 3.3 (0.9), meat 19 (0.5), and poultry 24 (0.8). For 228 Ra the intake is half or less than that of 226 Ra. Most of the naturally occurring b activity in food can be attributed to 40 K …127  109 y) (0.0117 at. %). A typical pair of approximate values [Bq=kg and (nCi=kg) ] is 25±74 (0.7±2). A few of the foods with higher speci®c

14. THE NUCLEAR ENVIRONMENT

581

activities are bananas 130 (3.5), spinach 222 (6), and coconut 222 (6). For growing plants, the availability of potassium is subject to large variation. Depending on the nature of the soil, only a small percentage of the potassium in the soil may be exchangeable and, therefore, available. In the United States the daily dietary intake of the b emitter 210 Pb (22.6 y) (uranium series) is about 37 mBq=kg (1 pCi=kg).

14.4.6 Materials Used for Building Construction Buildings can provide some shielding from extraterrestrial radiation and from g radiation from rocks and soil outside the buildings. However, certain materials of construction (e.g., stone, especially granite), containing uranium or a high potassium content, can raise the dose of ionizing radiation received by the occupants of a building. In the 1950s it was shown that the concentration of radon could reach 11 kBq=m3 (30 pCi=liter) in the air of a residence that was heated by radiant heating from concrete ¯oors containing crushed Chattanooga shale having about 0.008% uranium. In Florida, phosphate rock (ore), which can contain about 0.004% uranium, is mined for the production of fertilizer. Conversion of the ore to fertilizer reduces the concentration of uranium and its decay product 226 Ra in the fertilizer. However, use of the mill tailings as ®ll around basements of buildings has resulted in elevated radon levels. In addition gypsum, CaSO4
2H2 O, a by-product that may be contaminated with 226 Ra, is used to manufacture plaster of paris and wallboard for building construction. Finally, cinder blocks manufactured from coal ash containing 226 Ra also are a potential source of radon in houses and other buildings. In the United States, following World War II, uranium was mined in 10 states: Arizona, Colorado, Idaho, New Mexico, North Dakota, Oregon, Pennsylvania, Texas, Utah, and Wyoming. Some of the approximately 24 million tons of tailings, a ®ne silt produced in the mining and milling of the ore, was used in several western states in concrete and as ®ll around the foundations of at least 5000 buildings that included private residences, schools, and public and commercial buildings. A similar situation occurred in Ontario Province in Canada. In the tailings that remain after the uranium has been leached from the ore, the 226 Ra activity can be as high as 37 37 MBq=kg (0.10±1.0 mCi=g). Concrete made from the tailings not only raised the level of g radiation, but also provided a concentrated source of radon within the buildings. Remedial action has been very costly. Treatment of mill tailings as radioactive waste is discussed in Section 14.12.2.4.

582

14.5 APPLICATIONS OF NATURALLY OCCURRING STABLE NUCLIDES AND RADIO NUCLIDES

14.5 APPLICATIONS OF NATURALLY OCCURRING STABLE NUCLIDES AND RADIO NUCLIDES TO THE STUDY OF THE EARTH AND ITS ENVIRONMENT 14.5.1 Types of Application The many environmental applications of naturally occurring nuclides can be separated into three categories. The ®rst category is the well-known use of isotopes as tracers. An example is measurement of the ratio of radiogenic, stable 87 Sr to stable 86 Sr to trace the source of groundwater and its path in an aquifer. Another is the use of cosmogenic 7 Be (53.28 d) as a tracer for river sediment and its resuspension. The second category includes the study of chemical and physical processes associated with events and changes that are occurring or have occurred in and on the earth and in its atmosphere. Differences in chemical or physical properties associated with differences in the masses of the isotopes of an element result in isotope fractionationÐa change in the relative abundance of isotopes of a given element. (See Chapter 13, Section 13.2.2.1.) Since isotope fractionation can be related to the environmental conditions on the earth when a change or event occurred in the past, it can be used as a research tool in atmospheric chemistry, geochemistry, paleogeology, paleoclimatology, and other ®elds related to the paleoenvironment. The third category encompasses studies to determine the age of materials, date events that occurred in the past (e.g., for geochronometry), or measure the rates at which changes (e.g., climatic changes) have occurred, using radioactivity as a nuclear clock or chronometer. The length of time measured by radiometric dating may be from a few years to the age of the earth. Commonly, a study in the second category will also include the use of radionuclides to establish the time when the process or event being studied occurred. Another method of determining the age of an ancient rock, sand, or objects buried in soil, for example, is based on a clock that measures the time interval since the undisturbed sample was last exposed to heat or sunlight. Time is proportional to the absorbed dose of ionizing radiation received by the sample from natural sources of ionizing radiation during the time interval. When the sample is heated or exposed to a laser, it emits light called thermoluminescence or optically stimulated luminescence, the intensity of which is proportional to the dose and, therefore, the exposure time (assuming the dose rate is constant). Luminescence occurs when electrons that were detached from atoms by the ionizing radiation and became trapped in imperfections in the crystal lattice of the material are given suf®cient thermal energy to become free. The potential energy stored in the crystal is emitted as light. The concentration of trapped electrons also can be measured by electron spin resonance (ESR) techniques. Data obtained by the various methods have been used in the formulation of models of naturally occurring processes (e.g., climatic changes) and in the

583

14. THE NUCLEAR ENVIRONMENT

testing of existing mathematical models and hypotheses. Such models are intended to enable prediction of future changes in the earth's environment. 14.5.2 Isotope Fractionation Because isotope fractionation (Section 13.2.2.1) is very small, except for 1 H and 2 H, any effect on the normal chemical behavior of an element is usually ignored. However, when a change in the ratio of two isotopes occurs in some process in the environment, the change can be used to obtain very valuable information about the environment, especially the paleoenvironment. Extremely small changes in the abundance ratio of two isotopes of an element can be measured very accurately by mass spectrometric methods using a variety of ultrasensitive mass spectrometers. The following are examples of such processes: photosynthesis of complex organic compounds, biological processes, and physical processes such as vaporization of a liquid, diffusion of a gas, and transport across the boundary of two phases. Isotope fractionation may have a temperature coef®cient large enough to permit use of the coef®cient as a paleothermometer to measure the temperature and temperature changes on the earth's surface (seawater and ice) over a very long period of time or at the time of a major environmental event in the past. An emerging method for studying the sources and fate of organic pollutants in surface and groundwater systems utilizes compound-speci®c stable isotope measurements of isotope fractionation of H, C, N, and Cl in compounds accompanying transport, metabolism, and biodegradation. The method uses gas and liquid chromatography and high-precision stable isotope mass spectrometry. The difference between the isotopic composition of an element in two samples of a material is commonly expressed in terms of the change in the ratio of numbers of atoms of two isotopes (e.g., 18 O=16 O). When the isotope ratio for an element in a sample of interest is compared with that in a standard sample, the difference between the ratios is usually expressed in terms of delta, d (values expressed in ``per mil''). For example, d18 O is de®ned by the equation d18 O ˆ

…Rsample †=…Rstd †  1000 Rstd

…14-4†

where R ˆ …18 O=16 O†.13 The following are a few examples of isotope fractionation: 1. Water in leaves of plants is enriched in where the plants are growing. 13

18

O relative to water in the soil

Standard mean ocean water (SMOW) is an example of Rstd for d18 O.

584

14.5 APPLICATIONS OF NATURALLY OCCURRING STABLE NUCLIDES AND RADIO NUCLIDES

0

5

10

Thousands of years before present 15 20 25

30

35

40

18

O (per mil)

−30 −35 −40 −45 −50

FIGURE 14-8 Variation of 18 O concentration in ice core samples from the Greenland Ice Sheet for the past 40,000 years. The abrupt change from a cold period to a warm period began about 11,650 years ago. The coldest periods in the North Atlantic are indicated by dots. From K. Taylor, Am. Sci.
, 320 (1999). Used by permission of Edward Taylor=American Scientist.

2. Photosynthesis in plants results in preferential uptake of 12 C so that biomass is depleted in 13 C relative to the atmospheric CO2 . In limestone,therefore, carbon-in-carbon inclusions formed by living organisms differ in their d13 C from the inorganic carbon. The value of d13 C varies with temperature. As little as 20 pg of carbon is required for mass spectrometric analysis. 3. Nitrous oxide emitted from soil is depleted in 15 N and 18 O relative to the values for atmospheric N2 O. 4. Stratospheric CO2 , O3 , and O2 are enriched with respect to 18 O relative to their isotopic composition in the atmosphere. 5. The isotopic composition of phosphate in vertebrate bone depends on the temperature when the bone was formed. The 16 O content is higher at higher temperature. 6. When ice forms in the ocean, it is enriched in 16 O relative to water. 7. Both snow and rain are enriched in 18 O. The enrichment increases with increasing temperature at the time of precipitation. 8. Atmospheric CO2 is enriched in 14 C relative to deep-water CO2. 9. An example of the use of the temperature dependence of d18 O to study the temperature pro®le of ice cores from the Greenland Ice Sheet over the past 40,000 years is shown in Figure 14-8. An abrupt change in climatic conditions occurred about 11,650 years ago. The time when this change began, which has been associated with a change in the behavior of the Gulf stream, can be pinpointed within about 20 years. It is not known whether anthropogenic activities can trigger a change in the way the Gulf stream transports warm water. 10. When atmospheric ozone is formed, the isotopic composition (18 O=17 O) is not that expected from the mass effect and is referred to as a ``massindependent'' effect.14 14

Y. Q. Gao and R. A. Marcus, Science, , 259 (2001).

585

14. THE NUCLEAR ENVIRONMENT

14.5.3 Radiometric Methods for Age Determination Both primordial and cosmogenic naturally occurring radionuclides in the environment can be used as nuclear chronometers to determine the dates of a wide variety of processes and events in the earth, on the earth and in the earth's atmosphere. The radiometric method of determining the age of a material is based on equation (13-14), which is rewritten here as follows: NA ˆ NA0 exp …

lA t†

…14-5†

where NA is the measured number of atoms of a radionuclide A in a sample at the unknown decay time t (the age of the sample), lA is the known disintegration constant of A, and NA0 is the number of atoms of A present when the sample became a closed system at time t0 .15 Time t is then the length of time that the clock has been ticking since t0 . If NA0 is known (as it is, e.g., for 14 C) the calculation is straightforward in principle, but not necessarily in practice. If NA0 is unknown (as is usually the case), there are several ways to evaluate it. In general, NA0 can be calculated from NB , the number of atoms of a single decay product, from NC , the number of atoms of a long-lived decay product in a naturally occurring series, or from ND , the stable end product 206 Pb, 207 Pb, or 208 Pb of a series. The corresponding equations are A ! B…s†

…14-6†

A ! C ! D…s†

…14-7†

Branched decay must be taken into account if it is signi®cant. When the decay of A is represented by equation (14-6), NA0 can be calculated from NA0 ˆ NA ‡ NB

…14-8†

where NB is the measured number of atoms of B formed in the sample by decay of A.16 Thus NB =NA ˆ exp …lA t†

1

…14-9†

and

15 Until recent years the procedures for measuring time by radioactive decay involved the measurement of the residual radioactivity of the decaying radionuclide. It is dif®cult to measure accurately the activity of very long-lived radionuclides with very low speci®c activity, by counting the nuclei that decay (a very small fraction of the total nuclei of the isotope). Mass spectrometric methods provide a direct measurement of the total number of atoms of an isotope in a sample and, therefore, require smaller sample size and can provide greater sensitivity. 16 Equation (14-8) is based on the assumption that NB0 is zero; otherwise a correction must be made.

586

14.5 APPLICATIONS OF NATURALLY OCCURRING STABLE NUCLIDES AND RADIO NUCLIDES


 1 NB tˆ ln 1 ‡ lA NA

…14-10†

Natural lead also contains a small amount of a fourth stable isotope, Pb(s), which is not radiogenic. If a sample contains lead that is partially primordial (with a known isotopic composition measured in samples containing no parent radionuclide) and partially radiogenic, a correction for the primordial lead can be made by expressing the amounts of radiogenic lead relative to that of 204 Pb. Samples containing uranium will contain the members of both the uranium and the 235 U (actinium) series. Both series can be used to measure time (as an internal consistency check). Similarly, the thorium series can be used separately or with one of the other series. The ratios of stable lead isotopes such as 207 Pb=206 Pb for the uranium and the actinium series vary with time and also can be used to determine the age of a sample. A nuclear method of chemical analysis commonly used to determine the concentration of an element in a geological material is isotope dilution analysis. In general, the method is useful when methods of quantitative separation of an element are not suitable. A known quantity (a spike) of a stable isotope of the element is added to a sample of the material having a known isotopic ratio for the added isotope. From the change in the ratio in a pure sample separated from the mixture and containing only a fraction of the total amount of the element of interest in the mixture, the total amount can be calculated. For other types of samples (e.g., biological), radioisotopes can be used. In one procedure, for example, a known quantity of the appropriate chemical species of the element of interest that is labeled with a radioisotope and has a known speci®c activity is added to a sample to be analyzed. From the decrease in speci®c activity of a pure sample separated from the mixture, the total amount of the element initially present in the sample can be calculated. Even before modern instrumental techniques became available and before all the members of the three naturally occurring series had been identi®ed, radioactivity was used to estimate the age of the earth17 from the 238 U and 4 He content of a uranium mineral. For a uranium-containing sample that is in secular equilibrium, eight a particles are emitted for each decaying 238 U. Unfortunately the 238 U=4 He method is not very accurate because of the ease with which helium can escape from a rock sample. When the uranium series (Figure 13-5), for example, is not in secular equilibrium in a sample, the members of the series are said to be in disequilibrium. A solid sample with cracks and a porous solid are examples of materials that would very likely lose gaseous 222 Rn and cause disequilibrium. In natural waters such as ocean water, disequilibrium is normal and can be attributed to 204

17

About 46  109 years, based on modern radiometric methods of dating. The age of the universe is about 13  109 years.

587

14. THE NUCLEAR ENVIRONMENT

the aqueous chemistry of the daughters of 238 U. Speci®cally, 234 Th (24.10 d) and 230 Th (754  104 y) [both as Th(IV)] are readily removed from ocean water by adsorption on particulate matter such as ocean sediment. Similarly, 222 Rn can escape into the atmosphere from surface water, and 226 Ra can be removed by incorporation in CaCO3 during formation of the shells of marine organisms. Much remains to be learned about the natural water chemistry of the elements that are members of the three natural series. Disequilibrium can be the basis for further study of the aqueous chemistry of these elements and for the study of chemical and physical processes in the environment. Fission track counting is one of several methods that can be used instead of mass spectrometric analysis to determine the age of uranium-containing mineral specimens. The method is based on measuring the number of tracks of ®ssion products per unit area of sample produced by the spontaneous ®ssion of 238 U (Section 13.5.4). After the tracks have been counted, the sample is irradiated with thermal neutrons to ®ssion some of the atoms of 235 U in the sample. From the number of new ®ssion product tracks and the neutron irradiation conditions, the number of atoms of 235 U can be determined. Then, from the known 235 U=238 U ratio and the known l for the spontaneous ®ssion of 238 U the age of the sample can be obtained. Age determination by the 40 K=40 Ar (40 Ar=39 Ar) method is useful for ages between a few thousand years and the age of the earth. The calculated age is relative to the last time the sample was heated and, therefore, lost some or all of the 40 Ar (s). Until 1966, the determination of the number of 40 K atoms in the sample depended on the dif®cult measurement of the very low speci®c activity of the long-lived 40 K …127  109 y†. In the improved method, the sample is irradiated with fast neutrons to convert 39 K (s) into 39 Ar (269 y) according to the nuclear reaction18 39

K…n, p†39 Ar

…14-11†

39

Next, the 40 Ar= Ar ratio is measured accurately by laser fusion (melting) mass spectrometrometry. From the number of 39 Ar atoms formed in the irradiation of the sample, the number of 39 K target atoms in the sample is calculated, and ®nally the number of 40 K atoms in the sample is calculated from the known ratio of 40 K to 39 K in normal potassium. Loss of 40 Ar before analysis is a potential source of error and varies with the type of sample. Correction for contamination by atmospheric Ar can be made based on the presence of 36 Ar (s) and the known ratio (295) of 40 Ar to 36 Ar in the atmosphere. Equation (14.5) is used in a different way for the determination of the age of a sample by the decay of the cosmogenic radionuclides 14 C (5715 y) and 3 H (12.32 y): NA is measured and NA0 is known. The age is the time since the 18

39

See Section 13.4.2, equation (13.27) and related footnote 19. Because of the long half-life of Ar (nuclide B), the number of atoms formed is …Rf †B multiplied by the irradiation time.

588

14.5 APPLICATIONS OF NATURALLY OCCURRING STABLE NUCLIDES AND RADIO NUCLIDES

source of the sample ceased to be in isotopic exchange equilibrium with 14 CO2 and HTO in the atmosphere. For example, in the case of 14 C it could be the time when a tree is cut down. Thus, after a tree is cut down, the ratio of 14 C to stable 12 C in a sample of wood from the tree decreases with the half-life of 14 C. The age of carbonaceous material (e.g., wood and cloth) can be determined by comparing the 14 C content of the material with that which the material had when it was part of a living system in equilibrium with 14 C in the atmosphere. In December 1949 Willard F. Libby introduced radiocarbon dating by using b-particle counting to measure the speci®c activity (disintegrations per second per gram of carbon) of the 14 C remaining in a sample. In 1977 a second method, in which the ratio 14 C=12 C is determined by accelerator mass spectrometry (AMS), became available. The measured ratio is NA in equation (14-5). This method, in which the atoms of 14 C are counted, can extend the useful time range somewhat, but, as for any radionuclide used for dating, the useful time range is primarily limited by the half-life of the radionuclide. The AMS method does, however, make possible the use of smaller samples (e.g., 10 3 times smaller: < 50 mg to a few milligrams of carbon) than the counting method. Ages up to about 70,000 years can be measured using AMS. Beta-particle counting of larger samples can be used for calibration. Radiocarbon dates are subject to many sources of error.19 Three were discussed in Section 14.4.3.1. Additional errors can arise from fractionation20 during the process whereby the 14 C was incorporated in the sample, and from contamination of the sample during preparation or analysis. Radiocarbon dates (or ages) have been calibrated by dendrochronology (dating of tree rings) combined with measurement of the 14 C=12 C ratio in the tree rings, by using other radionuclide dating systems, and by using historical data. Radiocarbon dates are usually reported as years BP (before present). This practice is based on taking the concentration of 14 C in the atmosphere as constant since 1950 (the present). At that time the half-life of 14 C was taken to be 5568 years and, prior to the testing of nuclear weapons, the average value of the natural speci®c activity of 14 C in wood was 255 Bq per kilogram of carbon (6.9 pCi=g C). Dates BP are on the same scale and can be compared. Conversion of a BP date to a calendar date (e.g., BC) is not simple because the atmospheric concentration of 14 C has not remained constant and the half-life of 14 C has been determined more accurately. The conversion requires a cali19

All applications of radiometric dating are subject to errors in addition to the usual experimental errors of measurement. Many errors result from assumptions that must be made about the system (e.g., that it has been a closed system and that it has not been contaminated). Additional errors may arise because the chemical behavior of the components is not fully understood. 20 A correction for fractionation can be made using d13 C, de®ned in terms of measured 13 C=12 C ratios as for d18 O in equation (14-4).

14. THE NUCLEAR ENVIRONMENT

589

bration, as mentioned earlier. From the change in 14 C concentration in the atmosphere later, it was determined that the residence time for 14 C as CO2 is about 4 years in the stratosphere and about 10 years in the atmosphere as a whole. An application of tritium dating that is environmentally relevant is measurement of the age of water in aquifers. When water is no longer in contact with the atmosphere as surface water, the 3 H content as HTO decreases from its equilibrium level, with a half-life of 12.32 y. Another example of the use of cosmogenic nuclides is to measure the buildup of 3 He, 10 Be, 21 Ne, 26 Al, and 36 Cl in the surface of rocks in a glacial moraine to determine how long the rocks have been exposed to cosmic rays.

14.5.4 Summary of Examples of Nuclides Used and Types of Application Table 14-3 contains examples of nuclides that have been used in the two categories of environmental applications in recent years. The radionuclides used to measure time are cosmogenic, primordial, or a daughter of the latter. Table 14-4 gives examples of chemical and physical processes occurring in the environment that have been studied. For examples of the types of system that have been studied to determine the age of a substance or the date when a particular event occurred in the past, see Table 14-5.

14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT: TYPES AND APPLICATIONS Special-purpose sources of ionizing radiation in the extended environment (not limited to the outdoor environment) range in size from low-level sources incorporated in consumer products used in the home to high-level sources located in industrial and medical facilities. Exposure to the radiation from such sources may be planned and based on risk±bene®t considerations (e.g., exposure of a patient resulting from a procedure in a medical facility), or it may occur accidentally in the workplace (e.g., exposure of a worker in a facility where special-purpose sources are used). The dose of ionizing radiation received from any of these sources will contribute to the total dose that a person receives in the course of everyday living. Other sources including nuclear reactors in central station power plants, nuclear weapons, facilities used to manufacture reactor fuel and weapons, and radioactive waste are discussed in Sections 14.7, 14.11, and 14.12, respectively.

590

14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT

TABLE 14-3 Examples of Naturally Occurring Nuclides Used for Studying Environmentally Related Reactions and Processes and for Radiometric Datinga Reactions and processesb 2

H=H or D=H He=4 He 10 Be 11 B=10 B 13 C=12 C 15 N=14 N 17 O=16 O 18 O=16 O 20 Ne=22 Ne 21 Ne=22 Ne 34 S=32 S 40 Ar=36 Ar 44 Ca=40 Ca 57 Fe=54 Fe 56 Fe=54 Fe 84 Kr=36 Ar 87 Sr=86 Sr 136 Xe=132 Xe 230 Th 3

124

Radiometric datingb H =3 He Be 14 C 14 12 C = C 14 13 C = C 26 Al 36 Cl =35 Cl 40 K=40 Ar, 40 Ar=39 Ar 87 Rb =87 Sr 92 Nb =92 Zr 129 127 I = I 129 129 I = Xe 146 Sm =142 Nd 147 Sm =143 Nd, 143 Nd=144 Nd 176 Lu =177 Hf 182 Hf =182 W 187 Re =187 Os 210 Pb 230 Th Ratios of members of the U, Ac, and Th series: 238  206 U = Pb, 238 U =230 Thc , 235 U =207 Pb 234  238 c 232 U = U , Th =208 Pb, 230 Th =232 Th , 230 Th =234 U , 226 Ra =230 Thc , 231 Pa =235 U , 207 Pb=206 Pb, 208 Pb=204 Pb, 208 Pb=206 Pb 207 Pb=204 Pb, 206 Pb=204 Pb 3

10

a10

Be, 14 C, 26 Al, and 36 Cl are cosmogenic radionuclides. are marked with asterisks (*). Relative to secular equilibrium ratio.

b Radionuclides c

TABLE 14-4 Examples of Studies of Chemical and Physical Processesa Atmosphere Changes in the temperature at the earth's surface during the last three decades Changes in N2 O concentration in the atmosphere Levels of CO2 in ancient times Rate of oceanic and terrestrial uptake of anthropogenic atmospheric CO2 Mixing of magmatic CO2 with atmospheric CO2 Exchange of soil carbon and carbon in atmospheric CO2 Chemistry of O2 , O3 , and CO2 (continues)

14. THE NUCLEAR ENVIRONMENT

TABLE 14-4 (continued) Gravitational enrichment of Kr and Ar Link between atmospheric CO2 concentration and global warming in the past Sources of sulfur and lead Biosphere Organic photosynthesis in sediments 28  109 years old Precursors of organic compounds found in sedimentary rock Body temperature of dinosaurs from d18 O in bone phosphate Living and dead carbon as sources of CH4 , CO, etc. Change in type of vegetation Uptake of atmospheric CO2 on land Isotope fractionation when polychlorinated biphenyls are dechlorinated by bacteria Climate Climatic conditions during the last glacial maximum Rapid and slow paleoclimatic changes History of glacial ice; glacial cycles Validity of the Milankovich hypothesis A warm period during relatively high solar radiance about a.d. 1000 Correlation between warming data from ice cores and climate changes in other regions of the earth Hydrosphere Groundwater: rate of mixing; transit time through an aquifer Ocean sedimentation rates Sources of wastewater Rise and fall of sea level in the past Changes in the isotopic composition of seawater in the past Changes in sea surface temperature (SST) Changes in subduction zones and mantle dynamics Instability of the Antarctic Ice Sheet Ocean circulation Paleotemperatures of the oceans Reduction of sulfate in seawater to form pyrite Variation in paleosalinity in estuaries Vertical mixing of ocean water (relevant to carbon cycle) Stability of methane hydrate El NinÄo in the past Correlation between changes in the California Current and glacial maxima Lithosphere Earth's mantle Geochemical processes: formation of igneous and metamorphic rocks; high-temperature metamorphism Volcanism, plate tectonics Weathering and erosion of the continental surface Chemistry of thorium at low concentrations in seawater Uranium series disequilibrium in basalts and magmas Formation and growth of clays Chemical exchange reactions between the earth's crust and its mantle Magmatic degassing of CO2 Continental weathering Earth's orbit: eccentricity a

Some examples may apply to more than one category.

591

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14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT

TABLE 14-5 Examples of Radiometric Age and Date Determinationa Biosphere Pollen in ice cores Evolution of fossil shells Layers of peat identi®ed with known paleoearthquakes Pollen, spores, seeds, microfossils, wood, and charcoal in peat to detect prehistoric earthquakes Permian±Triassic extinctions Climate Date of last glacial maximum Episodes of glaciation Geomagnetic ®eld Lava ¯ows that are studied to determine variations in geomagnetic paleointensity (affects production of 14 C by cosmic rays) Reversals of the geomagnetic ®eld Hydrosphere Sea shells Greenhouse gas (methane) hydrates in ocean sediments Coral deposits Sediments in freshwater lakes Deep water in the Arctic Ocean Well water Lithosphere Formation of the earth's crust Sedimentary rocks Geochronology of Yucca Mountain (proposed HLW repository) Mantle recycling Organic material trapped in glacial moraines Potassium-containing minerals Strata where fossils are found Regions where asteroid impacts have occurred Paleovolcanic events to determine suitability of sites for a geological repository for high-level radioactive waste Plate-tectonic events Lava ¯ow pulses separated by thousands of years Sul®de minerals Zircon crystals in volcanic rock and in sedimentary material Mantle plumes near oceanic islands Carbonates at archaeological sites Rocks and glacial moraines to determine their ``exposure age'' (i.e., length of exposure to cosmic rays) a

Some examples may apply to more than one category.

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14.6.1 Sources Used for Structural Analysis of Solids, Radiography, Diagnostic Imaging, and Medical Therapy 14.6.1.1 Focused-Beam Sources

X-ray machines and neutron sources are used in research to determine the spatial arrangement of atoms by x-ray diffraction and neutron scattering in crystalline solids, respectively. X-ray machines for dental and medical radiography are commonplace special-purpose sources of ionizing radiation. Both the x-ray machines and the associated photographic ®lm have been improved over the years to reduce patient exposure. X rays are also used for diagnostic imaging of soft tissue by computed tomography (CT) or CAT (computed axial tomography) scanning.21 The x-ray source rotates completely around the patient's body, resulting in a series of cross-sectional views. Data for x-ray transmission are processed with a computer, which provides a display of an image of the region of the body being scanned. Another type of CT scanner is the electron beam device (EBCT) in which pulsed beams of electrons strike tungsten targets arranged in a ring about the patient's body. The tungsten x rays (Figure 13-20) that are generated in the targets enable parts of the body (e.g., coronary arteries) to be observed in motion. It is appropriate at this point to call the reader's attention to a nuclear diagnostic technique, magnetic resonance imaging (MRI), that uses computer analysis of nuclear magnetic resonance (NMR) measurements (see Section 13.2.2.2) to produce diagnostic tomographic images of internal body tissue without exposing the patient to ionizing radiation.22 The most commonly used stable nuclide is 1 H. A variation of MRI called functional MRI (fMRI) is becoming widely used to provide tomographic images of neural brain activity. Changes in blood ¯ow in small regions of the brain can be identi®ed when the patient carries out a mechanical task, responds by visual recognition, responds to music, and so on. In this technique a radiofrequency excitation pulse increases the magnetic energy of the nuclei (protons) in the sample. The measured time (relaxation time) required for the pulse to decay exponentially as these nuclei return to their initial energy states depends on the magnetic properties of nuclei in nearby molecules. Since bound oxygen 16 O (spin ˆ 0) in blood affects the relaxation time, it can be used to measure blood ¯ow.

21 Tomography is the procedure in which a collimated beam of x rays or g rays is focused on a speci®c plane or ``slice'' of an organ or region of the body. Variations in density of tissue cause variations in the attenuation of the photons, which in turn cause corresponding variations in the output of the radiation detectors that provide the data. 22 MRI rather than NMRI is used because of the widespread fear of all things nuclear.

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14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT

Because it is desirable that every effort be made to reduce a person's exposure to ionizing radiation, other procedures for noninvasive diagnosis such as those using MRI or ultrasound may replace or supplement the use of x rays and g rays for certain types of medical diagnosis. X-ray machines and g-ray sources are also used for industrial radiography of metallic products to ®nd ¯aws, defective welds, and so on. After nuclear reactors became available for large-scale production of g-emitting radionuclides, 60 Co (5.271 y) and 137 Cs (30.07 y) replaced sealed radiographic sources containing 226 Ra (1599 y) and its daughters. Both x rays and the g rays from 226 Ra and its daughters have also been used as external sources of ionizing radiation for medical therapy. One or more highly collimated beams of g rays are directed at the area to be irradiated. Common sources of g rays in devices now used for cancer therapy include 60 Co and 137 Cs. As for radiographic sources, radiation therapy devices may contain terabecquerels (tens to hundreds of curies) of a radionuclide. Boron neutron capture therapy (BNCT) has been used with some success to treat inoperable brain tumors. The patient is given a boronated pharmaceutical that concentrates in the tumor and then the tumor is exposed to a beam of neutrons from a nuclear reactor. The products of the 10 B…n, a†7 Li reaction, 4 He‡ and 7 Li‡ , are ionizing and have a high linear energy transfer. Another procedure being investigated for cancer therapy is based on the use of an accelerator-produced beam of high-energy ions of elements such as neon, carbon, and silicon. The procedure requires that the beam of these high-LET ions be accurately focused on the site of the malignancy. 14.6.1.2 Implanted Sources Used in Medical Therapy

Ever since radium became available, small radioactive sources have been implanted in or near tumors to destroy them. Both 226 Ra (encapsulated in a needle) and 222 Rn (encapsulated in a glass or gold seed) have been used with limited success. Today, this type of radiation therapy, called brachytherapy, utilizes small rods, beads, seeds, or rice-sized pellets containing radionuclides emitting low-energy ionizing radiation such as 103 Pd (16.99 d, EC, e , x rays ˆ 21 keV), 125 I (59.4 d, EC, e , Eg ˆ 35.49 keV), 90 Y (2.67 d, b ), 192 Ir (73.83 d, EC, b , g rays, mainly 0.316 MeV) and 252 Cf (2.646 y, a, e , lowintensity g-rays and neutrons from spontaneous ®ssion). Because of the limited depth of penetration of the radiations from these radionuclides, the risk of irradiation of nearby healthy tissue is low. The availability of imaging methods and improved delivery techniques facilitates precise positioning of the implants. Examples of implant applications are 103 Pd and 125 I for prostate cancer and 90 Y for one type of liver cancer, hepatocellular carcinoma.

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Californium-252 is useful in brachytherapy for tumors as a neutron source rather than photon source. Neutrons have a higher quality factor (Q) or radiation weighting factor (wR ) than photons (Tables 13-7 and 13-8). A controversial application of ionizing radiation is intravascular therapy to prevent reclosing (restenosis) of coronary arteries after angioplasty. As one example of the techniques used, seeds containing a radionuclide such as 192 Ir or 90 Sr are placed in a catheter, which is positioned for a short time in the region from which the plaque was removed. 14.6.2 Sources Used in Nuclear Medicine In nuclear medicine, a radiopharmaceutical, also called an imaging agent or a tracer and containing a particular radionuclide in a speci®c chemical form, is administered orally or intravenously to a patient. Diagnostic imaging is the usual purpose but, less frequently, radiation therapy is performed.23 The radiation that is measured to obtain an image of an organ originates within the body rather than in an external source of x or g rays. Radionuclides suitable for diagnostic imaging decay by the emission of g rays that are detected by an array of detectors in a ``g-ray camera,'' which, in the simplest planar procedure, provides an image showing abnormalities in the region in which uptake of the radionuclide has occurred.24 Radionuclides that decay by isomeric transition and electron capture have the advantage of not exposing the patient to high-energy particulate radiation. Suitable radionuclides must also have a relatively short half-life (minutes to days) and be readily incorporated into a nontoxic radiopharmaceutical. A radiopharmaceutical contains a radionuclide in a chemical form that has been shown to concentrate in a speci®c organ (target organ) or region of the body. In a few radiopharmaceuticals, the radionuclide is present in a relatively simple chemical form. With few exceptions, the target organ of a radiopharmaceutical is not determined directly by the chemistry of the radionuclide, but by the chemistry of the organic or inorganic compound (e.g., an amino acid, a chelate, etc.) containing the radionuclide. Commonly used b - and g-emitting radionuclides are 51 Cr (27.702 d), 67 Ga (3.261 d), 99m Tc (6.01 h), 111 In (2.8049 d) 123 I (13.2 h), 125 I (59.4 d), 131 I (8.0207 d), 133 Xe (5.243 d), and 201 Tl (3.039 d). A few examples of speci®c radiopharmaceuticals and their 23

An organic compound such as CH4 in which a signi®cant fraction of the stable 12 C atoms have been replaced by stable 13 C or by radioactive 14 C or 11 C is an isotopically labeled compound. A compound such as Na99m TcO4 , sodium pertechnetate, is not labeled in the same sense because there is no stable isotope of technetium. In a more general usage, the word ``labeled'' indicates that the compound contains a stable nuclide or a radionuclide that makes the compound suitable for a particular use. 24 The camera is a g-ray detector with a specially con®gured shield of absorbing material to collimate the photons entering the detector.

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14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT

diagnostic applications are listed in Table 14-6. The structure of one of these, technetium-99m sestamibi, is shown in Figure 14-9. The levels of activity needed for diagnostic imaging vary from about 200 kBq to 750 MBq (5.4 mCi to 20 mCi). TABLE 14-6 Examples of Diagnostic Radiopharmaceuticals Radiopharmaceuticala Gamma-ray emitters 51 Cr-EDTA 67 Ga-citrate 99m TcO4 (Na‡ salt) 99m Tc-arcitumomab 99m Tc-DMSA 99m Tc-DTPA 99m Tc-MAA 99m Tc-MAG3 99m Tc-nofetumomab merpentan 99m Tc-pyrophosphate 99m Tc-labeled red blood cells 99m Tc-sestamibi 99m Tc-sulfur colloid 111 In-capromab pendetide 111 In-imicromab pentetate 111 In-labeled leukocytes 111 In-DTPA 123 I (Na‡ salt) 125 I-labeled antigen 131 I (Na‡ salt) 201 TlCl 133 Xe Positron emitters (annihilation photon emitters) 11 C-labeled compounds 11 C-palmitate 13 N-labeled compounds 13 NH3 15 O-labeled   compounds H2 15 O 18 F-labeled compounds 18 F-deoxyglucose 82 Rb (As Rb‡ ) a

Application

Renal tracer Tumor imaging Thyroid function, blood ¯ow, brain imaging Imaging recurrent and=or metastatic colorectal carcinomas Renal function Renal function Venous blood ¯ow Renal function Detection of small-cell lung carcinoma Bone imaging Spleen imaging Mycocardial perfusion imaging, imaging of breast lesions Liver imaging Detection of recurrent and metastatic prostate cancer Imaging damaged myocardial tissue Imaging infections Flow of cerebrospinal ¯uid Thyroid function Radioimmunoassay Thyroid function Myocardial perfusion Lung ventilation Metabolic studies Long-chain fatty acid metabolism Metabolic studies Myocardial perfusion Metabolic studies Myocardial perfusion Variety of studies Glucose metabolism Myocardial perfusion

EDTA, ethylenediaminetetraacetic acid; 99m Tc-arcitumomab, radiolabeled monoclonal antibody; DMSA, dimercaptosuccinic acid; DTPA, diethylenetriaminepentaacetic acid; MAA, macroaggregated albumin; MAG3, mercaptoacetylglycylglycine; nofetumomab merpentan, radiolabeled monoclonal antibody; sestamibi, 2-methoxyisobutyl isonitrile (Figure 14-9); 99m Tc sulfur colloid, Tc2 S7 ; capromab pendetide and imicromab pentetate, radiolabeled indium monoclonal antibodies.

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+

|||

|

|

|||

|

| |

|

|||

|||

|

|

R | N R ||| R N C N C | C Tc C | C N C N R R ||| N | R CH3 | R = –CH2 – C – O – CH3 | CH3

FIGURE 14-9 Sestamibi with 99m Tc.

Two special diagnostic procedures are known as PET and SPECT. In positron emission tomography (PET), the radiopharmaceutical contains a positron emitter. The method is based on the fact that when a positron is annihilated, two photons (0.511 MeV each) are emitted at 1808 to each other (see Section 13.7.1.3). The point of annihilation in three-dimensional space can be determined accurately by counting the photons that arrive in coincidence in a pair of detectors that are positioned at 1808 relative to each other. The pair of detectors can be rotated around the patient in a circular or oval path, as for CAT and MRI scanning, or the patient may be surrounded by an array of pairs of detectors. Computer-assisted reconstruction generates the images. PET is also useful for studying metabolic kinetics and blood ¯ow in the brain. Examples of positron emitters incorporated in radiopharmaceuticals are 11 C (20.3 m), 13 N (9.97 m), 15 O (122.2 s), 18 F (1.8295 h), 62 Cu (9.74 m), and 82 Rb (1.26 m). These radionuclides are produced with a dedicated particle accelerator, that is, apparatus located at or near the medical facility at which the positron emitters are used. Examples of production reactions are 12 C…d, n†13 N, 14 N…d, n†15 O, and 18 O…p, n†18 F. Table 14-6 gives only a few of the many compounds that are labeled with positron emitters. One positron-emitting imaging agent, 2-[18 F]¯uorodeoxyglucose (18 FDG or FDG), which has been used over the years for evaluation of glucose metabolism and myocardial viability, also has chemical properties that make it suitable for identifying cancerous tissue and detecting false indications of cancer obtained in standard tests. It, unlike a radiopharmaceutical designed to bind to cells of a particular organ, is nonspeci®c. That is, it will ®nd any cancerous

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tissue and detect metastases. The rapidly growing cells in such tissue have a higher need for glucose than normal cells and accept FDG as glucose only to ®nd that it is an unusable permanent resident. FDG is more effective for fast rather than slowly growing cancer cells. In single-photon emission tomography (SPECT), the camera or array of cameras rotates around the patient's body and provides data for reconstructing images of planes. This procedure provides images with greater contrast than those obtained with the planar procedure for the same radionuclide. Certain short-lived radionuclides used to prepare radiopharmaceuticals can be obtained from ``generators'' that are commercially available. These generators contain a relatively large amount of the longer-lived parent of the radionuclide of interest. The shorter-lived daughter grows [equation (13-23)] and is removed chemically as needed. An example is the separation by simple chromatographic elution of 99m Tc as the pertechnetate ion, 99m TcO4 , from the 99 Mo (2.7476 d) parent.25 Other generator-produced radionuclides include 62 Cu from 62 Zn (9.22 h) and 82 Rb from 82 Sr (25.36 d). Technetium-99m has been called the workhorse of nuclear medicine for several reasons: (1) there seem to be an endless number of 99m Tc compounds that can be used to target virtually any organ of the body, (2) its half-life is quite suitable, (3) its g-ray energy (142.7 keV) is ideal for measurement, and (4) it is readily available from a generator. The versatility of Tc arises from its electron con®guration (4d5 5s2 for the outer electrons in the ground state) and, therefore, oxidation states from 1 to ‡ 7. Although 99m TcO4 , the chemically stable form in which 99m Tc is stored in aqueous solution, mimics I and is itself used as a radiopharmaceutical, Tc(VII) is usually reduced to Tc(VI), Tc(IV), or Tc(III) before being combined with a ligand to form a radiopharmaceutical. In terms of the environment, it is of interest to note that 99m Tc decays into 99 Tc, a ®ssion product and a pure b emitter with a half-life of 213  105 y. Iodine-131 (8.0207 d), which concentrates in the thyroid, is used not only diagnostically but also therapeutically to treat patients with hyperthyroidism and other thyroid diseases, including cancer, and after thyroidectomy. The quantities of 131 I (as iodide) used for hyperthyroidism are about 222±333 MBq (6±9 mCi). Another radionuclide used for therapy is 32 P (14.28 d) (as orthophosphate). It is used in the treatment of polycythemia vera, a condition in which the patient's blood has an abnormally high concentration of red cells. The quantity administered [up to about 185 MBq (5 mCi)] is limited by the extent of allowable irradiation of the bone marrow. Additional examples of radionuclides that are used for radiotherapy (including radioimmunotherapy with labeled antigens to treat lymphoma and 25 Molybdenum-99 can be made by neutron irradiation of molybdenum [i.e., 98 Mo…n, g†99 Mo], or it can be separated from the other ®ssion products produced by neutron irradiation of a sample of 235 U.

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leukemia) are 89 Sr (50.52 d), 90 Y (2.67 d), 125 I (59.4 d), 153 Sm (1.928 d), 186 Re (3.718 d), 188 Re (16.94 h), 198 Au (2.6952 d), and 211 At (7.21 h). Yttrium-90 can be obtained as needed from a generator containing its parent, 90 Sr (28.78 y). The latter can be removed from ®ssion product waste accumulated from reprocessed, neutron-irradiated 235 U or 239 Pu. A radionuclide that is believed to show promise for destroying cancer by aparticle immunotherapy is bismuth-213 (45.6 m, b 97.8%, a 2.2%). The 213 Bi is attached to an antibody that in effect transports the radionuclide to the cancer cells. This therapy has been effective in destroying the cancer cells that remain after chemotherapy treatment of acute myeloid leukemia. The availability of 213 Bi is rather interesting. It is a member of the 233 U (1592  105 y) decay series, which terminates in stable 209 Bi rather than a lead isotope. It is the granddaughter of actinium-225 (10.0 d, a), which can be separated from 233 U and can then be used as a 213 Bi generator. Uranium-233, which has potential use in nuclear weapons or in fuel for nuclear reactors, has been made in kilogram amounts by neutron irradiation of 232 Th and is in storage awaiting disposal. It should be apparent that investigators with a good knowledge of the fundamentals and an interest in discovering new uses of radioisotopes for medical diagnosis and therapy, are limited only by ingenuity.

14.6.3 Multifarious Sources The following are examples of other sources of ionizing radiation in the environment:  For many years the oxides of uranium were used to produce orange or green glazes for tableware and other ceramic items that have become collectibles. The oxides are still used as pigments in cloisonne jewelry.  Uranium has been used to color glassware, and thorium has been incorporated as an impurity in yellow glassware containing cerium.  Radium is well known as the energy source in self-luminous devices. The radium content of the luminous paint used on the dials of men's wristwatches manufactured before 1960 varied between 3.7 kBq and 0.15 MBq (0.1±4 mCi). Exposure to the wearer of a wrist-watch with radium paint is reduced by absorption of the a and b particles and a fraction of the g rays by the watch case and works.  Tritium (12.32 y), which emits only low-energy negatrons (Emax ˆ 18.591 keV), and 147 Pm (2.6234 y), (b , Emax ˆ 224 keV, low-intensity g) are used as substitutes for radium in luminous paint. Up to 930 MBq (25 mCi) of 3 H and 7.4 MBq (200 mCi) of 147 Pm are used for watches and clocks. These two radionuclides are used in a variety of other products containing

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self-luminous paints or plastics. Although there is no risk of skin exposure to b radiation from tritium in a watch, a watch with a plastic back rather than a metal back can allow tritium to diffuse through the back and then to be absorbed through the skin. The glass capsules used in night sights for ®rearms contain about 1.85 GBq (50 mCi).
Tritium is also used in sealed tubes in exit signs, miniature light sources, and so on in amounts up to about 1.1 TBq (30 Ci). Krypton-85 (10.76 y), (b , Emax ˆ 687 keV, low-intensity g) is used in similar applications.  Tritium, 85 Kr, 147 Pm, and 63 Ni (100 y) (b only, Emax ˆ 669 keV) are used in electronic devices, ¯uorescent lamps, and so on in amounts from 0.37 kBq to 3.3 MBq (0.01±90 mCi).  Alpha particles from 241 Am (432.7 y) are used to ionize the air in one type of smoke detector that is designed for use in any type of building but is especially suited for early detection of residential ®res. Smoke particles attenuate the steady ionization current reaching the detector and trigger an audible alarm. These battery- or ac-operated devices are small, can be attached to a ceiling, and are not considered to be a radiation hazard. They may contain up to 925 kBq (25 mCi) of 241 Am.  Polonium-210 (138.38 d), an a emitter, 3 H and 241 Am have been used in antistatic devices.  A wide variety of radionuclides are routinely used as tracers in many ®elds of research. Radionuclides are available in pure form and in labeled compounds, some of which are very complex and are synthesized by animals. Hundreds of 14 C-labeled compounds and many compounds labeled with 3 H, 32 P, 35 S, and 125 I are commercially available. Included are products such as labeled antigens used in radioimmunoassay (RIA), mentioned in connection with nuclear medicine.  Radioisotope thermoelectric generators (RTGs)26 that utilize radioactive decay heat have been developed to supply power for space vehicles and satellites, remote terrestrial systems such as polar weather stations, seismic sensing stations, navigational buoys, and so on, and implanted cardiac pacemakers. The two radionuclides that have been used most often are 238 Pu (87.7 y) and 90 Sr (28.78 y). Plutonium-238, an a emitter with Ea ˆ 54992 MeV (71.1%) and 5.4565 MeV (28.7%) for the two important a particles and low-energy, very low intensity g rays, is the preferred power source for space applications and pacemakers. It has a power density of 0.55 W (thermal) per gram of 238 Pu, requires very little shielding, and can be incorporated in generators providing tens of kilowatts of power. Strontium-90 sources require relatively heavy shielding, largely because of the relatively high-energy

26

RTGs were originally called systems for nuclear auxiliary power (SNAP).

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b radiation and associated bremsstrahlung from the 90 Y daughter (Figure 13-13). The power density for 90 Sr is 0.93 W per gram of 90 Sr.  Small radioisotope heater units (RHUs) also containing 238 Pu as the dioxide are used to heat instruments and equipment used in experiments conducted in spacecraft. A unit contains about 2.7 g of the fuel, weighs about 40 g, and provides heat output of 1 watt.  Direct energy conversion also has been used to obtain electrical energy from radioisotopes. Electrical power output of the order of microwatts is obtained by absorbing the ionizing radiation in a semiconductor material such as silicon, thereby generating a direct current for applications requiring polarity and negligible current.  Over 30 small nuclear reactors with electrical power output in the order of kilowatts have been used in satellites placed in orbit by the former Soviet Union (FSU). Radiation from these space reactors has created serious interference with satellites designed to study g rays in space, especially g rays associated with solar ¯ares.  Thickness gauges using radionuclides are used in industry to measure and automatically control the thickness of products such as paper and sheet metal. As the material passes between the radioactive source and a radiation detector, it absorbs some of the radiation. Variations in thickness cause variations in the signal output of the detector. What appeared to be a malfunction of a thickness gauge containing 137 Cs in a plant making sheet steel led to the accidental discovery of 60 Co contamination in the plant's steel supply.  Accelerators and nuclear reactors of several types are operated in research centers and in facilities used for the production of radioisotopes for use in research laboratories, medical facilities, and so on. Air that is used for ventilation in buildings containing accelerators that produce neutrons can contain short-lived radionuclides such as 16 N (7.13 s), 17 N (4.17 s), and 19 O (26.9 s), as well as the longer-lived 41 Ar (1.83 h). The neutron-activated air is generally exhausted through a high stack, so that the radioactivity is diluted to an acceptable level before it reaches the ground.  Gamma-ray sources containing 60 Co or 137 Cs and particle accelerators are used commercially to produce radiation-induced changes in a variety of materials. Chemical effects that occur when a substance absorbs ionizing radiation constitute the branch of chemistry known as radiation chemistry. As in photochemistry, free radicals play an essential role in the radiation± chemical reactions that occur in an absorber after an initial interaction. Radiolysis, the decomposition of compounds by ionizing radiation, is discussed in Chapter 13 (Section 13.8) for the case of water. The three most common, cost-effective applications at this time are sterilization of packaged medical supplies, irradiation of food (Section 14.6.3.2), and modi®cation of polymers (e.g., cross-linking of polyethylene). Cobalt-60 sources used

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for sterilization of medical supplies, for example, contain from a few peta becquerels to 2 EBq (a few tenths to about 5 MCi). Particle accelerators include positive ion accelerators, but most are electron accelerators having an electron energy range of 3±10 MeV. Radioisotopes or accelerators or both are in use as sources of ionizing radiation in over 40 countries.
Electron accelerators are used to irradiate material with electrons or with photons (bremsstrahlen). Because electrons have a limited depth of penetration into an absorber, they are suitable for producing a radiationinduced effect in the surface region of the absorber. Small electron accelerators can be used to decontaminate biologically contaminated pieces of mail.
A particular type of electron accelerator, the synchrotron, has become very popular as a research tool. A synchrotron accelerates electrons to very high energies (e.g., 1 GeV) as they travel along a circular path determined by a magnetic ®eld. Unlike the electrons in a linear accelerator, which emit photons when suddenly stopped in a target, the electrons in a synchrotron continually emit low-energy photons that can have an energy up to about 25 keV and can be removed from the accelerator as a ``bright,'' coherent beam of X rays. This type of accelerator is referred to as a ``synchrotron light source.'' The photons are especially useful for protein crystallography, structural biology, structural genomics, studies of interacting molecules, surface chemistry, and environmental chemistry. There are over 40 synchrotron light sources in use worldwide, and about two dozen more are under construction or planned.
The following are examples of processes that are in various stages of research and development for using ionizing radiation to remove environmental pollutants: (1) Treatment of the gaseous ef¯uents (¯ue gas) from fossil-fueled power plants to enhance removal of sulfur dioxide and oxides of nitrogen. Irradiation of a mixture consisting of the gas, water vapor, and ammonia leads to the formation of solid ammonium sulfate and ammonium nitrate that can be mechanically removed from the gas before it is discharged. (2) Sterilization of sewage sludge used in agriculture. (3) Degradation of a wide range of potential pollutants consisting of organic chemicals, including dichlorobiphenyl, contained in aqueous industrial waste. (4) Puri®cation of water drawn from municipal water supplies. These processes utilize the radiolysis products of water and require doses of tens of kilograys.

14.6.3.1 Neutron Activation Analysis and Thermal Neutron Analysis

Neutron activation analysis (NAA), a nondestructive method of quantitative chemical analysis, is based on equation (13-27). The unknown number of

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603

target atoms of an element of interest is NA in Chapter 13 (Section 13.4.2, footnote 19). When a sample is irradiated with slow neutrons, the stable nuclei of some of the constituent elements will become radioactive, usually by the (n, g) reaction. Ideally, the quantity of a radionuclide produced can be determined by quantitative measurement of its characteristic radiation, by g-ray spectroscopy, without the need for chemical separation from radioisotopes of other elements. NAA has been used for the determination of about 60 chemical elements in concentrations ranging from that of a bulk component to that of a trace component at the parts-per-million to parts-per-billion level. The sensitivity for a trace element depends on the neutron activation cross section of the target nuclide and on the properties of the product radionuclide (i.e., the halflife, and type, energy, and intensity of the radiation emitted). Examples of determinations of trace concentrations in environmental samples are Cu and Mn in both raw and treated water supplies, Cl in pesticide residues, rare earth elements contained in cracking catalysts used in oil re®neries and released into the atmosphere in particulate form, and a system of several elements (e.g., As, Sb, Se, Zn, In, Mn, V) present in atmospheric pollution aerosols and having the relative concentrations characteristic of their sources. A variation of NAA is based on measurement of the characteristic energies of the prompt g rays emitted by the target nuclei as the neutron capture reactions occur. It is advantgeous for the analysis of H, B, C, N, and Si. One application, known as thermal neutron analysis (TNA), was developed to detect chemical explosives in luggage at airports. Most chemical explosives have a relatively high nitrogen content. When nitrogen is irradiated with slow neutrons, the reaction 14 N(n, g)15 N releases a 10.8-MeV g rayÐan easily detected signature for the reaction. The intensity of the g ray is proportional to the nitrogen concentration. Several TNA detectors were built (using 252 Cf as the neutron source) and were tested with limited success (excessive false alarms). Changes in the design of devices using neutrons may eventually give them a signi®cant security role. 14.6.3.2 Food Irradiation

Food irradiation, sometimes called ``cold pasteurization'' or ``electronic pasteurization,'' is ®nding increasing worldwide use. This use of ionizing radiation has been endorsed by the UN Food and Agriculture Organization (FAO), the World Health Organization (WHO), and the International Atomic Energy Agency (IAEA). Its use has been approved in over 40 countries, about 30 of which now irradiate a variety of products up to a total of 60. Belgium, France, and the Netherlands are among the countries that have established markets for irradiated food. In the United States, however, food irradiation is a controversial topic

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14.6 SPECIAL-PURPOSE SOURCES OF IONIZING RADIATION IN THE ENVIRONMENT

(as was the pasteurization of milk for some 30 years). Because of fear, not cost, the process is not yet used to a signi®cant extent even though millions of cases of foodborne illness might be ameliorated by irradiation, and indeed approximately 10,000 food-related deaths are reported annually, with the risk of such fatalities apparently increasing. Growing public concern about foodborne illness has raised the level of interest in the bene®ts of irradiation. Examples of the types of food product for which processing with ionizing radiation has been developed include wheat, to disinfect insects; spices and seasonings, to kill microorganisms and insects; fresh fruits and vegetables, to delay maturation; carrots, potatoes, onions, and garlic, to inhibit sprouting; fresh ®sh, shell®sh, and frozen ®sh, to extend shelf life; pork, to control trichinosis; poultry, to control Salmonella and Campylobacter; and red meat, especially ground beef, to control Listeria and E. coli. Worldwide disinfection of spices by irradiation increased from about 6000 metric tons per year in 1987 to about 80,000 metric tons in 1998. The U.S. Food and Drug Administration (FDA) approved irradiation of pork in 1985, poultry in 1990, and ground beef in 1997. Several of the examples just cited illustrate how irradiation of certain foods can be used to reduce the dependence on chemical pesticides and fumigants. Irradiated spices are produced commercially in at least 12 countries. When food is irradiated, it is placed on a conveyor belt and moved past a source of ionizing radiation. The source may provide a beam of high-energy electrons (an e-beam source); x rays, including bremsstrahlen; or g rays from a radioactive source sealed in a double-walled, stainless steel container. The source of g rays is usually 60 Co but may be 137 Cs. Packaging material may require use of the more penetrating radiation from 60 Co. The dose of ionizing radiation (g radiation from radionuclides or bremmstrahlung from electron accelerators) used for food irradiation ranges from a few hundredths of a kilogray to about 50 kGy, depending on the objective. To inhibit sprouting and to kill insects and parasites, the required dose is usually less than 1 kGy. Extension of shelf life (by about 2±3 weeks) for normal methods of storage and removal of microorganisms that cause spoilage requires a higher dose (e.g., up to about 10 kGy). For sterilization of food for long-term storage at room temperature, a dose of about 50 kGy is used in combination with heat. Food consumed by astronauts receives a dose of 25 kGy or more. An interesting radiation-resistant bacterium, Deinococcus radiodurans was found in 1956 in radiation-sterilized meat products. It is also found in soil, dust, and many other places. It has an extraordinary ability to repair DNA damage caused by high doses of ionizing radiation (1.5 million rads), especially in the absence of water. It is over 100 times more resistant to ionizing radiation than E. coli. It may have potential in radioactive waste treatment.

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At high dose levels, radiation±chemical (radiolytic) changes in food not only can have an adverse effect on color and ¯avor (e.g., changing the ¯avor of dairy products and introducing rancidity in food with high fat content) but also can cause partial loss of vitamins. These deleterious effects can be reduced by vacuum-packing the food to remove oxygen and freezing it before irradiation, a practice that reduces the formation of substances by reaction of the radiolysis products of water (Section 13.8) with the chemical constituents of food. Radiolysis of the complex molecules in food also produces free radicals that can react to form a wide variety of molecules known to be mutagenic or carcinogenic. These are the same compounds that are introduced when food is processed without ionizing radiation (e.g., by cooking) and are, therefore, normally present in processed food. Those opposed to food irradiation believe that irradiation makes the food unsafe. However, the Joint Expert Committee on the Wholesomeness of Irradiated Food of the World Health Organization (WHO), representing several international organizations, reached the conclusion that the irradiation of any food up to an overall dose of 10 kGy causes no toxicological hazard and introduces no special nutritional or microbiological problems. This dose will not produce sterile foods of the type needed by people who are diagnosed as having compromised immune systems. Apparently, ionizing radiation does not destroy food-borne viruses. Irradiation of food with g rays from radioactive sources does not make the food radioactive. As pointed out in Chapter 13, when ionizing radiation from such sources interacts with the atoms of an absorber, food in this case, it transfers a portion or all of its energy to the absorber, including the parasites or bacteria. The incident radiation is not stored in the absorber. Accelerator-produced, high-energy bremsstrahlen (> 8 MeV) can be absorbed in photonuclear reactions [e.g., …g, n†, …g, p†, and …g, a†]. The cross sections (probabilities) for these reactions are relatively small except for photon energies corresponding to resonance absorption. For some of the isotopes of the light elements (isotopes with an odd number of neutrons, e.g., 2 H, 13 C, and 17 O), the binding energy of a neutron is less than 5 MeV; hence, the (g, n) reaction is possible for bremsstrahlen used for food irradiation. Although the products of the (g, n) reactions for these three nuclides are not radioactive, the neutron released in each case will be captured by some stable nuclide in the food and may produce a radionuclide by the (n, g) reaction. Based on the chemical elements normally present in signi®cant amounts in food, the only radionuclide that might reach a detectable level by neutron capture for an irradiation dose of 10 kGy is 24 Na (14.95 h). In the United States, the Food and Drug Administration (FDA) and the Department of Agriculture (USDA) set the requirements for approval of new uses. The FDA, which establishes the rules for labeling food, requires that irradiated food be labeled and show the international logo, called a radura

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FIGURE 14-10 The radura, the internationally recognized logo for irradiated food.

(Figure 14-10). Accompanying the radura must be a statement such as ``Treated with Radiation'' or ``Treated by Irradiation.'' The size of the type used for labeling and the requirement itself have been part of the food irradiation controversy. The solid circle of the logo represents an energy source; the two petals (green, when colored) represent the food; and the ®ve breaks in the circle represent radiation from the source. There is some concern that use of the logo and the accompanying statement could encourage careless handling during subsequent processing and preparation of the irradiated food, which has no protection against bacterial contamination and must be refrigerated after removal from its sealed container. The FDA has placed regulatory limits on the energy and the dose of radiation that can be used for the irradiation of food for human consumption, animal feed, and pet food, and on the packaging materials for irradiated food.27 Examples of the irradiation limits that apply to food for human consumption are given in Table 14-7.

14.7 NUCLEAR FISSION POWER PLANTS Nuclear power reactors are of environmental concern for three major reasons. One is the release of radioactive nuclides during normal operation or accidentally. A second is the problem of disposal of spent fuel and other contaminated material. A third is the possibility of nuclear fuel being diverted to weapons. Before these can be discussed, it is necessary to discuss the reactors themselves with respect to types and the fuels they use.

27

Code of Federal Regulations, Title 21, Part 179, Food and Drug Administration (HHS), U.S. Government Printing Of®ce, Washington, DC (revised annually).

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TABLE 14-7 Limitations on the Use of Ionizing Radiation for the Treatment of Food Purpose Control of Trichinella spiralis in pork Growth and maturation inhibition of fresh food Disinfestation of arthropod pests Microbial disinfection of dry or dehydrated enzyme preparations Microbial disinfection of speci®ed dry or dehydrated vegetable substances used in small amounts for ¯avoring or aroma, (e.g., spices, herbs, etc.) Control of food-borne pathogens in fresh or frozen uncooked poultry products Sterilization of frozen, packaged meals used solely in the NASA space program Control of food-borne pathogens in and extension of shelf-life of refrigerated or frozen, uncooked meat or meat by-products or meat food products composed solely of intact or ground meat, meat by-products or both meat and meat by-products For control of Salmonella in fresh shell eggs For control of microbial pathogens on seeds for sprouting

Dose limitationsa±c Min 0.3 kGy (30 krad) Not to exceed 1 kGy (100 krad) Not to exceed 1 kGy (100 krad) Not to exceed 1 kGy (100 krad) Not to exceed 10 kGy (1 Mrad) Not to exceed 30 kGy (3 Mrad)

Not to exceed 3 kGy (300 krad) Min 44 kGy (4.4 Mrad) Not to exceed 4.5 kGy for refrigerated products Not to exceed 7.0 kGy for frozen products Not to exceed 3.0kGy Not to exceed 8.0 kGy

a

The following radiation sources can be used for the inspection of food, for inspection of packaged food, and for controlling food processing: x-ray tubes with 500 kV peak or lower; sealed units producing radiations at energy levels of not more than 2.2 MeV from the isotopes: 241 Am, 137 Cs, 60 Co, 125 I, 85 Kr, 226 Ra, and 90 Sr. Californium-252 neutron sources used for moisture measurement in food have additional limitations. b Conditions for using ionizing radiation for safe treatment of food: sources of ionizing radiation are limited to (1) g rays from sealed units of the radionuclides 60 Co or 137 Cs, (2) electrons generated from machine sources at energies not to exceed 10 MeV, and (3) x rays generated from machine sources at energies not to exceed 5 MeV. c For a food, any portion of which has been irradiated in accordance with regulations, the label and labeling and invoices or bills of lading must bear the statement ``Treated with radiation (or by irradiation)Ðdo not irradiate again.'' Source: Based on Code of Federal Regulations, Title 21, Part 179, Food and Drug Administration (HHS), 2001.

14.7.1 Types of Nuclear Power Reactor Several types of nuclear ®ssion reactor have been used as heat sources to generate steam in power plants. A power reactor may be identi®ed in different ways. For example, it may be a thermal or a fast reactor, depending on the energy of the neutrons causing ®ssion (see Chapter 13, Section 13.7.3). A thermal reactor is usually identi®ed according to the neutron moderator used. If the moderator and coolant are different, both are speci®ed. Table 14-8 lists characteristics used to identify power reactors. Almost all nuclear power reactors in operation worldwide at the time of writing are thermal reactors; that is, ®ssion is induced when 235 U captures a thermal rather than a fast neutron. Thermal power reactors using H2 O as both

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TABLE 14-8 Characteristics Commonly Used to Identify Nuclear Power Reactors Characteristic Fissile material Moderator Coolant Neutron spectrum Fertile material

Examples 233

U, 235 U, 239 Pu H2 O, D2 O, C (graphite) H2 O, D2 O, molten Na, CO2 , He Slow (thermal), intermediate, fast 238 U, 232 Th

moderator and coolant are known as LWRs (light water reactors), those using D2 O as HWRs (heavy water reactors). LWRs, the most popular type in most countries, are further subdivided into PWRs (pressurized water reactors) and BWRs (boiling water reactors). Nuclear reactors are also classi®ed in terms of the way ®ssile material is used and formed. A reactor that uses highly enriched uranium as fuel without fertile material is a ``burner.'' A nonmilitary research reactor is an example, although most of these devices have been modi®ed to use fuel with no more than 20% 235 U. A ``converter'' is a reactor that burns one type of ®ssile nuclide (e.g., 235 U) and makes another (e.g., 239 Pu) but makes less fuel than it burns. LWRs are converters. Breeder reactors produce more of a given ®ssile material than they ®ssion.

14.7.2 Nuclear Fuel The methods of processing uranium ore and enriching the uranium for production of nuclear reactor fuel were developed in the nuclear weapons program and are discussed in Section 14.11.2. Most nuclear power reactors in operation at the time of writing use a fuel consisting of uranium that is slightly enriched in 235 U (e.g., 2±4% of the uranium vs 0.720% in natural uranium) and is known as low-enrichment fuel (LEU), fuel having less than 20% of the uranium as 235 U. As the 235 U is ®ssioned, some of the 238 U is converted to 239 Pu by the successive steps given in equation (13-44). A fraction of the 239 Pu ®ssions and contributes to the energy output of the fuel.28 A fraction captures neutrons to form not only 240 Pu and higher isotopes of plutonium but also isotopes of transuranic elements with higher atomic number by a series of neutron capture and decay steps. The concentrations of these nuclides increase with increasing irradiation time. 28

By the time the irradiated fuel has been removed, about half the ®ssion energy is coming from plutonium.

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Plutonium in the irradiated fuel can be chemically separated by reprocessing and then used as a reactor fuel. When used as a fuel, the plutonium is usually mixed with UO2 to form a mixed oxide known as MOX and containing 3±5% Pu. The UO2 is made from depleted uranium (DU), the uranium that remains in the 235 U enrichment process and has a 235 U content below the 0.720 at. % in natural uranium. Although MOX is required for fast reactors, it can also be used in LWRs and HWRs (described shortly) after some modi®cation of the reactors. It has been used in Belgium since 1963. France, Great Britain, Japan, and Russia have programs involving MOX. MOX is being used in nuclear power plants to reduce the amount of weapons-grade plutonium now being stored (Section 14.11.6). Another fuel (®ssile nuclide) that has been used on a demonstration scale is 233 U. It can be made according to equation (13-45). By means of the 232 Th 233 U fuel cycle, the predominant, fertile isotope of thorium in nature could be used in the future to generate power. Either 235 U or 239 Pu would have to be used to make the initial supply of 233 U by neutron irradiation of thorium. Almost all power reactors in operation in the 1990s contained the fuel in the form of cylindrical pellets of LEU UO2 enclosed in a thin-walled metal tube (cladding) to form a fuel element or rod or pin (Figure 14-11a). Zircaloy, an alloy of zirconium, is commonly used for the cladding.29 Zirconium has a low absorption cross section for thermal neutrons, but it does react with water and steam at high temperatures to produce hydrogen. Fortunately, a protective ®lm of ZrO2 prevents it from reacting with H2 O during normal reactor operation. The rods are mounted in an assembly (Figure 14-11b) which may contain between 36 …6  6† and 306 …17  18† rods. The assembly has a width between 13 and 30 cm, a length between 4 and 4.5 m, and contains from about 180 to about 460 kg of uranium, depending on the type of reactor. A reactor core consists of an assembly of fuel assemblies in a structure that allows for the passage of control rods and the ¯ow of coolant.

14.7.3 Nuclear Fuel Requirements A ®ssion rate of 31  1010 ®ssions per second will provide 1 W of power (thermal). For a power plant with a thermal output of 3000 MWt as heat or an electrical output of about 1000 MWe of electricity the number of 235 U nuclei that must be ®ssioned per second is 93  1019 .30 This corresponds to the ®ssioning of 3.1 kg of 235 U per day. Uranium in spent fuel contains about 0.8 w % 235 U. 29

Zircaloys are alloys of zirconium and tin with minor constituents. MWe indicates the rate at which electrical energy is generated and MWt indicates the rate at which thermal energy is generated. MWe is about 30% of MWt for nuclear power plants with watermoderated, water-cooled reactors. (Note: in much of the literature, the symbols MWe and MWt are used without supscripts.) 30

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14.7 NUCLEAR FISSION POWER PLANTS

(a)

(b)

FIGURE 14-11 (a) Fuel rod containing uranium dioxide pellets. (b) Assembly of fuel rods. From The Harnessed Atom, U.S. Department of Energy, DOE=NE-0073.

The fuel rods must be replaced periodically, not only because of partial depletion of the 235 U, but also because of buildup of ®ssion products that are neutron absorbers, distortion of the pellets as each 235 U atom is replaced by two atoms of other elements, and stress cracking of the cladding. The extent to which fuel can be irradiated before being replaced is expressed in terms of ``burnup'': MWd=MTHM (megawatt-days per metric ton of heavy metal as LEU uranium before irradiation). Variations in expressing burnup include the use of MWDT (megawatt-days thermal), MTIHM (metric tons of initial fuel loading), MWd/t, GWd/t (t ˆ metric ton), and TJ/kgU. For light water reactors (described in Section 14.7.4.1.1), typical burnup in the past has been 30,000±40,000 MWd=MTHM with refueling (replacing

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one-third or less of the fuel) every 12±18 months. Increased burnup (e.g., 55,000 MWd=MTHM), resulting in longer time period between refueling shutdowns, has been achieved in many nuclear power plants in various ways, including improved fuel element design. Fewer and shorter outages (reduced from 30±50 days to about 20 days) for refueling and maintenance have improved the capacity factor and the economics of plant operation. The capacity factor for a speci®ed period of time is the percentage of design (maximum) power output actually achieved.

14.7.4 Types of Nuclear Power Plants 14.7.4.1 Pressurized Water Reactor Power Plants 14.7.4.1.1 LWR Plants

First developed for the propulsion of submarines and other naval vessels, PWRs are much more compact than the graphite-moderated reactors used in the nuclear weapons program during World War II.31 The PWR type of reactor was also a logical choice for central power stations because its compactness made possible the use of relatively small containment buildings and because the electric utilities were experienced in the use of liquid water and steam in their fossil-fueled power stations.32 In pressurized water reactors the water that is pumped through the core containing the fuel rods is under pressure (about 15 MPa) to prevent its boiling. Hydrogen is injected into this primary loop to suppress the formation of oxygen by radiolysis of the water and thereby prevent the oxygen concentration in the core from reaching a value high enough to make an explosive mixture. The water (at about 3168C) in the primary loop is pumped through steam generators (e.g., four), where heat that has been removed from the core is transferred to water to generate steam in the secondary coolant loop as shown in the simpli®ed schematic diagram of Figure 14-12. Steam (at about 2608C and 5.5 MPa) goes to a steam turbine. Any radioactivity present in the primary coolant from activation of corrosion and erosion products or ®ssion products escaping from defective fuel rods does not contaminate the steam unless leakage occurs from the primary coolant in the steam generators (SGs). Leakage through cracked tubes carrying the primary coolant in the steam generator has been a problem for PWRs. The number of such tubes is commonly over 3000 in a 350-ton SG that may be 31 The ®rst nuclear-powered (PWR) naval vessel was the submarine USS Nautilus, which was launched in 1955. 32 The ®rst central station, commercial nuclear power plant in the United States was built in Shippingport, Pennsylvania, and began operation in 1957. The reactor was a PWR and the electrical output was 90 MWe.

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14.7 NUCLEAR FISSION POWER PLANTS

Pressure relief Pressurizer valve (PRV)

Borated water (ECCS) Nitrogen under pressure (ECCS) Borated water

Steam generator

Steam

Control rods

Core

Electrical generator

Turbine

Pump

Secondary loop

Pressurized primary loop

Condenser

Reactor vessel

Water

Cooling water Pump

Feedwater heater Pump

Pressurized water

Pump

Containment building

FIGURE 14-12 Simpli®ed schematic for a pressurized water reactor (PWR) nuclear power plant.

about 60 ft long and about 15 ft in diameter. The entire reactor complex, with its control rods, primary loop, pressurizer that maintains pressure in that loop, emergency core cooling system (ECCS), and steam generators, is located in a specially designed containment building constructed of reinforced concrete (about 1 m thick) and having a steel liner (about 0.4 m thick). The purpose of the containment building is to prevent the release of radioactivity into the environment if the reactor is involved in a steam or chemical explosion. The version of a PWR developed for use in submarines and in power plants in the former Soviet Union is known as the VVER (Russian acronym for water±water power reactor). 14.7.4.1.2 HWR Plants33

Pressurized heavy water power reactors using D2 O as both moderator and coolant were developed in Canada and are known as CANDU (ada 33

The reactors are also referred to as PHWRs.

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613

euterium $ranium) reactors. In HWR plants D2 O under pressure is circulated through pipes containing the fuel in the core and then through primary loops and heat exchangers, where it transfers heat from the core to H2 O in the steam generator. Because D2 O is a better neutron moderator than H2 O, the fuel is natural uranium rather than the LEU used in LWRs. Unlike the LWRs, the HWRs are designed so that they can be refueled without being shut down. 14.7.4.2 Boiling Water Reactor Power Plants

As the name implies, the water that removes the heat from the reactor core of the boiling water type of LWR is allowed to boil and generate steam directly within the core.34 The steam thus generated (at about 2888C and 10 MPa) is used directly to drive the turbine. Steam is delivered to the turbine via a steam separator and a drier that removes the liquid from the water±steam mixture leaving the reactor. Volatile ®ssion products that escape from any defective fuel rods are carried with the steam to the steam turbine. Devices such as catalytic recombiners are incorporated in a BWR system to prevent dangerous buildup of hydrogen and oxygen produced by the radiolysis of water in the core. Two containment systems are used to prevent release of radioactivity in the event of an accident in a BWR plant. The primary containment is a steel pressure vessel that surrounds the cylindrical reactor vessel and is itself surrounded by reinforced concrete. The building that houses the reactor and the primary containment vessel is constructed of reinforced concrete and constitutes a secondary containment layer. Any radioactive material that escapes from the primary containment vessel is con®ned within the secondary containment space. 14.7.4.3 Water - Cooled, Graphite Moderated Reactor Power Plants

The ®rst-ever nuclear power station (5 MWe) was built in the USSR and began operation in 1954. Its reactor was fueled with uranium metal (5% 235 U), moderated with graphite, and cooled with pressurized water that ¯owed through a primary loop and then through a heat exchanger to generate steam in a secondary loop. Later (in the 1970s), large boiling water, pressure tube, graphite-moderated high-power boiling channel reactors were built for both the production of Pu and the generation of power. This type of reactor, called RBMK after the Russian acronym, has fuel rods consisting of UO2 (enriched to about 2% 235 U) in Zircaloy cladding and control rods that move within channels in the graphite. Water ¯ows around the fuel rods in vertical channels and is allowed 34

The core of a BWR plant with an electrical capacity of 1000 MWe contains about 125 metric tons of LEU as UO2 .

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14.7 NUCLEAR FISSION POWER PLANTS

to boil and generate steam in the core. In a 1000-MWe RBMK (RBMK-1000), the steam goes to two 500-MWe generators from two halves of the reactor that can be operated separately. The RBMK was the most popular type of civilian power reactor in the Soviet Union prior to the Chernobyl accident in 1986 (see Section 14.16.2.3). These reactors can be refueled while operating, and they allow the use of low-enrichment fuel. Although large water-cooled, graphite-moderated reactors had been operated safely in the United States from the time of the Manhattan Project in the 1940s until 1994, they were used primarily for the production of Pu for nuclear weapons. Some also generated electricity, but as a type of reactor, they were never developed for use in U.S. commercial power plants. The last of these, the N Reactor at the Hanford Reservation in Washington State (near Richland), began operation in 1963 and was permanently shut down in 1986 after the Chernobyl accident. Although these reactors had many design features to make them safer than the RBMKs, they lacked a major safety feature, namely, a containment building. 14.7.4.4 Gas-Cooled, Graphite Moderated Reactor Power Plants

Gas-cooled (CO2 ), graphite-moderated reactors (GCRs) using natural uranium and a magnesium alloy (Magnox) as cladding and advanced gas-cooled reactors (AGRs) using LEU fuel (UO2 ) have been used in power plants in the United Kingdom for many years. These power plants, which generate steam, operate at higher temperatures than do LWRs. A different type of graphitemoderated, high-temperature, gas-cooled reactor, the HTGR, has been studied in Germany and in the United States for many years. Pressurized helium was the coolant. Uranium carbide (UC2 ) or oxycarbide (UCO) initially containing 235 U in the form of coated microspheres was the fuel, and coated microspheres of ThO2 served as fertile material for the production of ®ssile 233 U by reaction (13-45). Eventually, such a reactor would operate on the 233 U 232 Th fuel cycle. The helium transferred heat from the core to a steam generator at a temperature of about 7008C, providing a higher thermal ef®ciency than that for an LWR. Further improvement of ef®ciency was planned by going to a gas± turbine cycle. The core of the HTGR was very different from that of an LWR. It consisted of an assembly of hexagonal graphite blocks containing vertical holes through which the helium could ¯ow and holes for rods containing the microspheres, coated with a layer of graphite, a second coating of silicon carbide, and another coating of graphite. Fission products were retained in the microspheres by the coating. A demonstration or prototype reactor (40 MWe) was built in Peach Bottom, Pennsylvania, and a second commercial 330-MWe plant, built at Fort St. Vrain, Colorado, operated with many outages for mechanical problems for

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about 10 years beginning in 1979. Development of the HTGR in the United States was terminated in 1994. Two HTGRs operated in Germany have been shut down. The reason for describing the HTGR is that the concept has been revived in South Africa, where the pebble bed modular reactor (PBMR) is being developed. As designed, the reactor is cooled by helium that leaves the reactor at about 9008C and generates electricity through a direct-cycle gas turbine. Each module has an output of only 110 MWe. The core contains about 400,000 pebbles (about the size of tennis balls), each of which contains about 15,000 seeds of enriched uranium as UO2 coated with layers of carbon and silicon carbide. The steel vessel containing the core is lined with graphite. The design allows spent fuel to be removed from the bottom of the core (into storage below the reactor) and new fuel to be added at the top without shutting down the reactor. A small (10-MWt), helium-cooled, pebble bed reactor began operation in China in 2000. It is designed as a source of process heat for industry and a source of electricity. 14.7.4.5 Sodium-Cooled, Fast Breeder Reactor Power Plants

Fast breeder reactors, known as liquid metal fast breeder reactors (LMFBRs), use 239 Pu as the ®ssile nuclide, 238 U as the fertile material, and fast rather than thermal neutrons. Reactors of this type have been built and operated in France, Japan, the former Soviet Union, the United Kingdom, and the United States to demonstrate their feasibility and to gain experience in their operation. The largest LMFBR power plant built up to mid-1998 is the 1240-MWe SuperPheÂnix located at Creys-Malville, France. These reactors are called breeders because they are designed to produce more 239 Pu than they ``burn'' by ®ssion. They can breed with 239 Pu as the ®ssile material because 239 Pu has a larger cross section than 235 U for ®ssion with fast neutrons and because the neutron absorption cross sections for ®ssion products and for structural and other materials in the core usually decrease with increasing neutron energy, making a larger fraction of the neutrons released in ®ssion available for converting 238 U to 239 Pu. One fuel that has been used in fast reactors is MOX containing about 20% PuO2 and about 80% UO2 . Stainless steel is a suitable cladding material for the fuel rods. Depleted uranium as UO2 also is used as a blanket around the core so that 239 Pu is produced in both the core and the blanket. Water cannot be used to cool the core of a fast reactor because it would function as a neutron moderator as well as the coolant. Sodium is not a good neutron moderator, and its physical properties make it a suitable coolant.35 35

Lead has been proposed as a substitute for sodium.

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14.7 NUCLEAR FISSION POWER PLANTS

It has a melting point of 98.78C and a boiling point of 8838C. As liquid sodium passes through the core, 23 Na captures neutrons to form 24 Na (14.95 h) and 22 Na (2.604 y) by (n, g) and (n, 2n) reactions, respectively. The coolant is, therefore, highly radioactive quite apart from any contamination by ®ssion product leakage from fuel elements. Sodium is spontaneously ¯ammable in air and must be handled in an inert atmosphere. Furthermore, it reacts violently with water to liberate hydrogen, which generally ignites. Although the technology for using molten sodium as a coolant is not new, sodium leakage problems have plagued operation of the few sodium-cooled power reactors that have been built.36 Most, including the SuperPheÂnix and one in Japan following a sodium ®re have been shut down at the time of writing. In one type of fast reactor (pool type), the core is immersed in a pool of molten sodium, which is circulated through the core by pumps located in the pool of sodium. Hot sodium (about 5008C) also is pumped from the pool through a primary loop and an intermediate heat exchanger, where heat from the pool is transferred to nonradioactive sodium in a secondary loop. Specially designed heat exchangers having double-walled tubes to prevent accidental contact of the sodium with the water are then used to transfer heat from the nonradioactive, liquid sodium to water and generate steam. In the second type of fast reactor (loop type), molten sodium is pumped through the core as for a PWR. The heat is transferred to a second loop of sodium and then to a steam generator as for the pool type reactor. The pool type design has been more popular than the loop type. Breeding 239 Pu enables operation of nuclear power plants by utilizing 238 U, the most abundant isotope of uranium. Breeder reactors are seen as a means to energy independence by nations that must import their fossil and nuclear fuel. They are also seen as a potential source of material that could be used for nuclear weapons by terrorists and rogue nations. 14.7.4.6 Thermal Breeder Power Plants (LWBRs)

Breeding of nuclear fuel also can be achieved in an LWR by using 233 U as the ®ssile material and 232 Th as the fertile material. The nuclear power plant in Shippingport, Pennsylvania (footnote 32), was operated at a power level of 60 MWe (net) from 1977 to 1982 to demonstrate the feasibility of breeding of 233 U in an LWR. Much of the technology that will be needed in the distant future when the 233 U 232 Th fuel cycle becomes a competitive source of energy is now known. 36 The second nuclear-powered submarine that was built in the United States, the USS Seawolf, was equipped with a sodium-cooled, beryllium-moderated reactor (not designed as a breeder). This submarine was launched in 1955.

617

14. THE NUCLEAR ENVIRONMENT

TABLE 14-9 Number of Nuclear Power Reactors by Type That Existed and the Number Operational Worldwide at the End of 2000 Type Pressurized light water Boiling light water Gas cooled Heavy water Graphite moderated, light water cooled Liquid metal, fast breeder

Total

Operational

289 98 32 52 14 5

256 92 32 43 13 2

490

438

Source: World list of nuclear power plants, Nucl. News, 44(3), 61 (2001) (revised annually).

14.7.4.7 Other

Several additional concepts for nuclear plants have been studied since the 1950s. Some were developed to the prototype stage, but all were abandoned. Three examples are the liquid metal fuel reactor (LMFR), a graphitemoderated device that had fuel consisting of uranium metal dissolved in liquid bismuth; the molten salt reactor (MSR), in which the uranium as a ¯uoride was dissolved in a eutectic mixture of the ¯uorides of Be, Zr, and Li; and the organic-cooled reactor (OCR), which contained a mixture of polyphenyls (high boiling hydrocarbon compounds) as substitute for water as coolant and perhaps as moderator. The ®rst two had materials problems related to containment of the fuel. Although polyphenyl compounds are relatively stable to radiolysis by ionizing radiation, they are not suf®ciently stable to survive in the intense radiation ®eld of a reactor core. Table 14-9 lists the types of nuclear power plant that existed and the numbers that were operational worldwide at the end of 1999.

14.7.5 Safety Features of Nuclear Power Plants 14.7.5.1 The Reactor

This section is intended to provide background information and insight that should be helpful for understanding what went wrong in two of the nuclear reactor accidents described in Section 14.16.2. The material has been simpli®ed (perhaps oversimpli®ed for some readers) in order to avoid a quantitative discussion of nuclear reactor kinetics.

618

14.7 NUCLEAR FISSION POWER PLANTS

The ®ssion rate and, therefore, the power level in a reactor, is controlled by rods that can be moved in or out of the reactor core. These control rods contain an element having at least one stable isotope that is a ``neutron poison'' (i.e., an isotope with a high absorption cross section for thermal neutrons). Examples are cadmium (113 Cd) and boron (10 B) as boron carbide. When the rods are fully inserted, the reactor is shut down. The reactor can be shut down by an operator or automatically by one of the engineered safety systems, if one of the various sensors in the core detects an unsafe condition (of neutron density, temperature, pressure, coolant ¯ow, etc.). Each type of power reactor has several intrinsic safety features. When a reactor is operating at a steady power level (steady ®ssion rate), the rate of production of ®ssion neutrons is equal to the rate at which they are absorbed in the core plus the rate at which they escape from the core. Absorption can be by H2 O,37 control rods, fuel-rod cladding, ®ssion products in the fuel, structural materials in the core, 235 U to cause ®ssion or to form 236 U, 238 U to cause ®ssion or to form 239 U (which is the source of the 239 Pu that accumulates in the fuel), and 239 Pu to cause ®ssion or to form 240 Pu. A safety-related question is, If the reactor is operating at full power and there is a temperature transient (e.g., a sudden increase in temperature of the water in an LWR, for example, because of a decrease in demand for steam or failure of a coolant pump and so on), how will the reactor respond? All the reactor parameters change with temperature. The cross sections for all the neutron reactions that can occur during the slowing-down process will change. Some will increase, others will decrease. Also, there will be density changes, especially for water. Analyzing this complex combination of changes shows that the overall temperature coef®cient for changing the power level for LWRs is negative and the reactors are stable. Therefore, if there is an increase in sudden temperature, the ®ssion rate will decrease until the temperature before the event is restored. A positive temperature coef®cient would lead to a continuously increasing temperature and an unstable reactor. Another question is, How will the reactor respond if a void is formed in the water of an LWR? Because a void is the absence of the neutron moderator, the number of thermalized neutrons will be insuf®cient to maintain a constant rate of ®ssion with themal neutrons. Thus, the void coef®cient (again, for the power level in this discussion) is negative and the ®ssion rate will decrease. One of the factors that contributed to the Chernobyl accident (Section 14.16.2.3) was the void effect. The type of reactor involved, an RBMK-1000 (Section 14.7.4.3), contains graphite to thermalize the ®ssion neutrons and 37

A good neutron moderator is ef®cient in removing kinetic energy from a fast neutron in each elastic collision, and it has a low cross section for absorbing a thermalized neutron. The order for thermalizing is H > D > C, i.e., decreasing order with increasing mass. However, when absorption is taken into account, the ranking order of moderators is D2 O > C > H2 O.

14. THE NUCLEAR ENVIRONMENT

619

boiling water as the coolant and minor moderator. A large voidÐone beyond that allowed for in the design (i.e., boiling water under pressure)Ðcreates a positive void coef®cient because it represents a removal of H2 O as an absorber of neutrons that have already been thermalized by graphite. This positive void coef®cient is not overweighed by the negative coef®cients for the other effects. Even though nuclear power plants have engineered safety features designed to prevent accidents by automatically and rapidly adding neutron poisons to shut down the reactor if a dangerous condition is detected, they are vulnerable to a type of accident that is not a problem for a power plant using a fossil fuel. After the reactor has been shut down, the core is still a large heat source (5±7% of full-power heat output).38 In fact, the decay heat generated in the fuel elements at the time of shutdown is more than suf®cient to melt the reactor core if, after a normal or emergency shutdown, the heat is not removed by continued pumping of coolant through the core. To provide emergency cooling, the power plant contains an engineered safety feature called the emergency core cooling system (ECCS), which is turned on automatically to remove the decay heat if the normal cooling system fails. Such a failure is called a loss of coolant accident (LOCA). If power for the ECCS from outside the plant (from the power grid) fails, diesel-operated generators are supposed to turn on within a few seconds to supply emergency power. We have not discussed the rate at which the power level of a reactor can rise. Fortunately, the delayed ®ssion neutrons slow the rate so that within de®ned limits of safe operation, the time available for adjusting the power level is reasonable. For details, see the additional reading and sources of information at the end of the chapter. 14.7.5.2 Dose Received by Workers

Obviously a nuclear power plant is a very complex system, with many regions containing sources of ionizing radiation. During shutdowns for refueling and so on, and during normal operation and maintenance, workers must follow set procedures to limit their exposure to values that are, hopefully, below those speci®ed in the operating license for the plant. During routine operation, workers must properly handle radioactive ef¯uents of the type described in the next section. The radiation dose received by workers at nuclear power plants in the United States has decreased steadily since 1980.39 For PWR plants the median value for the man-rem dose per unit decreased from 417 in 1980 to 82 in 2000. The corresponding change in dose for BWR plants was from 859 to 150. 38

As an example, for an LWR having a thermal output of 3000 MWt, a burnup of 33,000 MWd=MTHM, and a fuel load of 82 MTHM, the decay heat immediately after shutdown is about 160 MWt or about 5.4% of the operating power. 39 Nuclear News, %% (6), 39 (May 2001).

620

14.7 NUCLEAR FISSION POWER PLANTS

14.7.6 Ef¯uents from Nuclear Power Plants A nuclear power plant is obviously not a source of greenhouse gases. If a 1000MWe nuclear power plant is substituted for a coal-®red plant of the same size, the annual production of such gases is reduced by approximately the following amounts, depending on the composition of the coal and the type of pollution control equipment installed: about 7 million tons of CO2 , about 100,000 tons of SO2 , about 25,000 tons of NOx , and about 1500 tons of particulates. In addition, there would be about 1 million tons less coal ash. On the other hand, a nuclear power plant has its own characteristic ef¯uents that are of environmental concern. During normal operation of a light water reactor (LWR), the cooling (and neutron-moderating) water will accumulate the following. Gaseous radionuclides Dissolved or colloidal, radioactivated corrosion products of the elements Fe, Co, and Mn Any radioactive, nongaseous ®ssion products and actinide elements that have escaped from the UO2 fuel by way of imperfections in the cladding of the fuel rods Fission products from the ®ssion of traces of uranium contamination on the outside of the fuel rods The amount of radioactivity a nuclear power plant is allowed to release into the environment by discharge as gas through a stack or as contaminated water is restricted by its license. The systems for preventing excess discharge of gases are complex, with holdup tanks for compressed gas containing short-lived radionuclides, ®lters to retain particulate matter, and charcoal absorbers to remove radioisotopes of Kr and Xe. Table 14-10 shows the level of radioactivity for gaseous and liquid ef¯uents and for solid waste released annually from BWRs and PWRs over a span of 20 years (1974±1993). One can discern a number of trends in this period. In interpreting such data or similar data about nuclear power plants, the following facts must be kept in mind.
No two nuclear power plants of a given type are identical. As newer ones were built, the experiences gained in operating the older plants were incorporated in design changes and improved chemical treatment processes for radioactive waste. There are limits to how much an old ( 20 years) plant can be upgraded.  Fabrication techniques for fuel elements have improved fuel performance over the years.  The data were not normalized to take into account the energy output of each plant each year. A given plant may have been shut down for weeks or

621

14. THE NUCLEAR ENVIRONMENT

TABLE 14-10 Radioactive Materials (curies) Released from Nuclear Power Plantsa Boiling water plant Year Airborne ef¯uents Gases: ®ssion and activation Productsc Averaged Number of nuclear power plants 131 I and particulates Average Number of nuclear power plants Liquid ef¯uentsf Tritium Average Number of nuclear power plants Mixed ®ssion and activation productsg Average Number of nuclear power plants Solid wasteh Average Number of nuclear power plants a

1974

324,000 20 1.63 20

1993b

1974

1993b

861e 36

2624 25

372e 75

0.0187 40

17.2 18

17.2 31

18.3 18

0.339 31

728 21

Pressurized water plant

12,820 39

0.207 25

421 24 1.69 25 494 20

0.0039 75

488 73 0.476 74 1250 70

The reported releases are generally planned and in accordance with plant license. However, they include unplanned releases, perhaps from equipment failure, that are below ``accident'' level. b The last year an annual report was prepared. c BWR: Radionuclides. Major contributors: 41Ar (1.83 h), 85mKr (4.48 h), 87Kr (1.27 h), 88Kr (2.84 h), 133Xe (5.243 d), 135mXe (15.3 m), 135Xe (9.10 h), 137Xe (3.82 m), 138Xe (14.1 m). Relative amounts vary from plant to plant. PWR: Radionuclides. Major contributors: 3H (12.32 y), 41Ar (1.83 h), 85Kr (10.6 y), 85mKr (4.48 h), 87Kr (1.27 h), 88Kr (2.84 h), 131mXe (11.9 d), 133Xe (5.243 d), 133mXe (2.19 d), 135Xe (9.10 h). Relative amounts vary from plant to plant. d Per plant, based on arithmetical average. e Also, BWR: 25 Ci of tritium (data for 1993), PWR: 65 Ci of tritium (data for 1993). f BWR: Aqueous waste that is diluted with water (perhaps by a factor of 102 105 ) before discharge. Final volume, 109 1012 liters (data for 1993). PWR: Aqueous waste that is diluted (perhaps by a factor of 102 103 ) before discharge. Final volume, 109 1012 liters (data for 1993). g BWR: Radionuclides. Major contributors: 51Cr (27.702 d), 54Mn (312.1 d), 55Fe (2.73 y), 60Co (5.271 y), 65Zn (243.8 d), 137Cs (30.07 y). Relative amounts vary from plant to plant. PWR: Radionuclides. Major contributors: 51 Cr (27.702 d), 55Fe (2.73 y), 58Co (70.88 d), 60Co (5.271 y), 124Sb (60.20 d), 125Sb (2.758 y), 133Xe (5.243 d), 137Cs (30.07 y). Relative amounts vary from plant to plant. h BWR: Consists of contaminated ion exchange resin, ®lters, sludges, miscllaneous equipment, and irradiated components. Radionuclides. Major contributors: 51Cr (27.702 d), 54Mn (312.1 d), 55Fe (2.73 y), 58Co (70.88 d), 60 Co (5.271 y), 63Ni (100 y), 65Zn (243.8 d), 134Cs (2.065 y), 137Cs (30.07 y). Relative amounts vary from plant to plant. PWR: Radionuclides. Major contributors: 3H (12.32 y), 14C (5715 y), 51Cr (27.702 d), 54Mn (312.1 d), 55Fe (2.73 y), 58Co (70.88 d), 60Co (5.271 y), 63Ni (100 y), 95Zr (64.02 d), 95Nb (34.97 d), 125Sb (2.758 y), 134Cs (2.065 y), 137 Cs (30.07 y). Relative amounts vary from plant to plant. Source: Based data in Radioactive Materials Released from Nuclear Power Plants, 1993, NUREG/CR-1907, BNL-NUREG-51581, Vol. 14. U.S. Nuclear Regulatory Commission, Washington, DC. December 1995.

622

14.7 NUCLEAR FISSION POWER PLANTS

many months for refueling, routine maintenance, replacement of equipment, and so on, or it may have operated year-round.
There have been changes in NRC regulations requiring certain operational changes (e.g., the lowering of airborne radionuclides for BWRs).
Changes in radionuclide release over the years also can re¯ect change in plant management. Radionuclides in the primary coolant of a PWR can enter the secondary cooling system through imperfections in the many kilometers of tubing contained in the steam generators that are components of the cooling loops. Water is also withdrawn from the primary loops to remove corrosion products, and other contaminants. The aqueous ef¯uents are passed through ®lters and demineralizers (inorganic or organic ion exchangers) to remove radionuclides. Such treatment does not, of course, remove two of the radionuclides produced in LWRs, namely, tritium (12.32 y) and 14 C (5715 y). Tritium can be formed as a product of the rarely occurring ternary nuclear ®ssion reaction in the fuel and escape through imperfections in the cladding. It can also be formed in LWRs by the 2 H…n, g† 3 H reaction with deuterium in normal water.40 In pressurized water reactors its major source is the 10 B…n, t† 4 He reaction in boric acid, which is added to the primary coolant as part of the reactor control system. Carbon-14 is produced in an LWR mainly by the 14 N…n, p†14 C reaction on nitrogen or nitrogen-containing impurities in the coolant, moderator, or fuel. Carbon-14 is also produced to a lesser extent by the 17 O…n, a†14 C reaction.41 When the 14 C escapes through leakage of the coolant, it may be as 14 CO2 , 14 CO, or 14 CH4 . For a given type of power plant, PWR or BWR, the systems used to limit the amount of radioactivity in the ef¯uents have become more complex and ef®cient over the years. Because the steam going to the turbines in a BWR plant is generated in the reactor core, the turbines become radioactively contaminated, the challenge of limiting the radioactivity in plant ef¯uents is greater than for a PWR and, therefore, some of the ef¯uents tend to have a higher level of radioactivity.

14.7.7 Advanced Nuclear Power Plants for the Future The two major driving forces for improving nuclear power plants are economics and safety. Features that can be changed to improve the economics are lowering the cost of construction (dollars per kilowatt of capacity), and increasing the reliability, which will lower maintenance and operation costs 40

The composition of normal hydrogen, is 99.985 at. % for 1 H and 0.015 at. % for 2 H. In a graphite-moderated reactor the 14 C is produced by the 13 C…n, g† 14 C reaction.

41

14. THE NUCLEAR ENVIRONMENT

623

and raise the capacity factor. Other improvements relate to minimization of radioactive waste and nonproliferation of nuclear weapons. One class of advanced light water reactors (ALWRs), ABWRs and APWRs designed in the United States, have evolutionary improvements based on experience with existing LWRs. They are comparable in generating capacity to existing large LWR plants but are simpli®ed (fewer welds, less piping) and have better instrumentation. The ®rst ABWR [1315 MWe (net)] was built in Japan and began operation at the end of 1995. Canada has developed an evolutionary, standardized design AHWR, the CANDU 3. France and Germany have jointly developed an evolutionary design for the PWR, called the European pressurized water reactor (EPR), that is available for replacement of aging nuclear power plants. Advanced gas-cooled reactors (AGRs) have been built in the United Kingdom. These use enriched uranium instead of natural uranium as fuel and have concrete containment buildings. Another class of advanced plants using LWRs is characterized as having passive cooling and passive safety features. Plants of this type differ markedly from existing plants while still providing safeguards against sabotage and diversion of plutonium. They require less human action, have fewer or no moving parts such as pumps and valves, have more safety features, and require no power to operate the safety systems. The latter include gravity feed of water stored above the reactor and greater use of convective and radiative heat transfer. Plants being designed with passive systems are generally mid sized (e.g., about 500 MWe). Both types of ALWR are expected to bene®t from the incorporation of standardized components, which should lower construction time and costs and expedite licensing. Advanced gas-cooled and liquid-metal-cooled reactors also have been designed.

14.8 NATURAL FISSION REACTORS (THE OKLO PHENOMENON) Natural ®ssion, water-moderated reactors (at least 16) existed on the earth and were part of the environment about 1.96 billion years ago in deposits of uranium ore in the Oklo region near Franceville in the Gabonese Republic on the west coast of Africa. At that time the abundance of 235 U in the ore was about 3% (about that used in LWR reactors) instead of the current value of 0.720%. It is estimated that the reactors, which operated intermittently, had an operational life in the range of 5  105 106 years. Suf®cient uranium remains so that there is an interest in mining at least one of the reactor sites. The fossil reactors in the Oklo area have provided information that is helpful for understanding the probable behavior of high-level radioactive waste within a repository. Data have been obtained on the radiation damage

624

14.9 THERMONUCLEAR POWER PLANTS

of materials in and near the reactor zones and on long-term migration of 235 U, 239 Pu, and ®ssion products. For example:
About half the ®ssion product elements remained in the UO2 ore, which is analogous to spent reactor fuel.
For ®ve ®ssion products that migrated from one of the reactor zones, the relative retentions were in the order Te > Ru > Pd > Tc > Mo. Some of these were retained in peripheral rocks.
Most of the cadmium and tin escaped from the reactor zones.
The heavy rare earth elements are more mobile than the light ones.
The 239 Pu (2410  104 y) present after the reactors ceased to operate remained immobilized long enough to decay into 235 U.

14.9 THERMONUCLEAR POWER PLANTS Although power plants using controlled thermonuclear reactions (fusion reactions) as the heat source do not exist, progress is being made on generating and controlling fusion reactions and on developing concepts for fusion power plants. Because of the large quantity of deuterium (0.015 at. % of the hydrogen and present as HDO and D2 O) that is available in the earth's hydrosphere and because of the existence of well-established methods for increasing the deuterium content of water, nuclear fusion has the potential of providing an almost unlimited source of energy in the future. The relatively low ignition temperature of the D-T reaction [equation (13-38)] has made it the reaction of choice in the facilities where fusion research and development are being conducted, and it will most likely be used in the ®rst generation of fusion power plants. Ultimately, the two D-D reactions [equations (13-39) and (13-40)] would be used. Helium-3 is not an attractive fuel because its natural abundance is only 14  10 4 at. %, and it is more dif®cult to make by a nuclear reaction than 3 H. In a controlled fusion reaction, it is necessary not only to create the plasma of reactant nuclei, but also to stabilize and con®ne it at the proper density and temperature ( 108 K). Furthermore, for power generation, the energy output must be greater than the energy input needed to produce and con®ne the plasma. Two very different approaches to developing fusion power are being pursued. In the method that has been studied for the longer period of time, the plasma is contained in a vacuum chamber. The plasma can be produced by several methodsÐfor example, passing a high current through the gaseous mixture of reactants (ohmic heating) followed by magnetic compression, or ionizing the reactants ®rst and then injecting them into the device. Magnetic ®elds are used in a number of ways to con®ne the plasma within the reaction

14. THE NUCLEAR ENVIRONMENT

625

vessel and away from the wall, since there is no containment material that could survive the temperature of the plasma. The tokamak, ®rst built in the USSR, is an example of a device that uses magnetic con®nement of the plasma in a torus (a single doughnut-shaped vessel). Magnetic con®nement42 has been investigated in the United States and in the former Soviet Union for many years. In the future, it is likely that major research and development projects based on magnetic con®nement will be pursued abroad at the Joint European Torus (JET) and the International Thermonuclear Experimental Reactor (ITER) project, which is supported by Europe, Japan, and Russia and is scheduled to be completed and to demonstrate the feasibility of commercial fusion power by about the year 2013. The experimental facility is in Japan. An early variation of the tokamak was the stellarator, in which the coils for generating the magnetic ®eld are wound around the plasma chamber (torus) in the shape of a helix rather than a series of rings. Although study of the stellarator design was discontinued by most countries in the 1960s, a modern version of this device, known as the large helical device (LHD), is being developed in Japan. In the second method, which uses inertial con®nement, high-power lasers or sources of high-energy electrons or ions provide high-input energy in pulses lasting perhaps a microsecond or a nanosecond to irradiate and compress the fuel mixture (2 H2 and 3 H2 ). Con®nement is achieved by sealing the fuel in small pellets or microspheres that are about 1 mm or less in diameter and are made of glass, for example. Irradiation by converging, pulsed laser beams rapidly vaporizes the con®ning shell of the pellet, creating an implosion that increases the density of the fuel mixture and heats it to the ignition temperature needed for the reaction to become self-sustaining. This technology is being developed at the National Ignition Facility (NIF) at the Livermore National Laboratory in California, and in Japan. The fusion device, which will have about 190 converging lasers, will be used to study and develop inertial con®nement fusion as a source of energy and to provide a means for maintaining the stockpile of nuclear weapons without testing. For either method there are major materials problems to be solved, especially for the reactor vessel. At times articles have been written with misleading information, leading the reader to believe that a fusion reactor would be free of radioactivity. The ®rst-generation reactors will very likely contain large amounts of radioactive tritium (12.32 y). The D-T reaction releases neutrons that will carry most of the energy released to the reactor vessel, where the resulting heat will be used to produce steam. The neutrons will also produce radionuclides by (n, g) and (n, p) reactions with the various stable nuclides in 42

Produced by the magnetic ®elds generated by current ¯owing in coils wound around the torus and current ¯owing through the plasma.

626

14.10 COLD FUSION

the reactor vessel and will cause embrittlement of the vessel, as is the case for ®ssion reactor vessels. It is also likely that the heat will be removed by molten lithium and that the reactor will be surrounded by a lithium-containing blanket (possibly molten Li) where, as for the lithium coolant, neutrons will be used to produce tritium by the reactions 6

Li ‡ 1 n ! 3H ‡ 4 He

…14-12†

and 7

Li ‡ 1 n …very fast† ! 1 n …not so fast† ‡ 3 H ‡ 4 He

…14-13†

If deuterium is eventually used alone as the fuel, the D-D reactions will produce both neutrons and tritium. In any event, thermonuclear power plants are not expected to become a reality until the distant future, perhaps by 2050.

14.10 COLD FUSION In March 1989, a ripple of excitement swept the world when it was announced that the results of experiments were believed to show that the energy of nuclear fusion could be released as heat by simply electrolyzing a solution of LiOD in D2 O in a cell having a palladium cathode and a platinum anode. The energy output of the cell as heat was measured to be greater than the energy input. Since the experiments were carried out at room temperature, the process was referred to as ``cold fusion.'' The implications of an inexpensive way of harnessing the energy of fusion were almost beyond imagination, especially for nations without energy resources. The same experiments and variations of them have been carried out in laboratories in many parts of the world since 1989, but the original results have not been duplicated. Other effects that are not readily explained have been observed but they, too, cannot be repeated. When a small energy release is observed, neutrons, protons, tritons, helium nuclei, and g rays are not observed in the quantities expected from reactions (13-39) and (13-40). It becomes necessary to assume that a new nuclear reaction mechanism can occur when deuterium is absorbed in palladium or some other metal. In April 1989 a special 22-member Cold Fusion Panel was established by the Energy Research Advisory Board of the U.S. Department of Energy. The panel reached several conclusions, which can be summarized by the statement that there was no convincing evidence to support the reported experimental results.43 43

John R. Huizenga, ``Cold Fusion: The Scienti®c Fiasco of the Century'', University of Rochester Press, Rochester, NY, 1992.

14. THE NUCLEAR ENVIRONMENT

627

14.11 NUCLEAR WEAPONS The nuclear weapons programs that a number of nations have undertaken since 1945 have had signi®cant effects on our nuclear environment.

14.11.1 Types In the ®rst generation of nuclear weapons (``A-bombs''), the explosive energy came from the ®ssion of 235 U or 239 Pu. The main source of energy in a thermonuclear weapon (``H-bomb'') is a reaction such as the D-T reaction (13-38), which is triggered by energy from the ®ssion of 239 Pu. This type of weapon can be made to release much greater explosive energy than ®ssion weapons (i.e., in the megaton energy range) with a smaller release of ®ssion products per unit explosive energy.44 On the other hand, if an outer layer of 238 U is added, the quantity of ®ssion products increases, and the weapon has been called ``dirty.'' By the end of the Cold War, the arsenal of nuclear weapons contained a variety of types ranging from heads for intercontinental ballistic missiles to relatively small tactical weapons. Reduction in the size, weight, and amount of ®ssionable material was made possible by incorporating deuterium and tritium in the weapons. Tritium was also used in the so-called neutron bomb. Because 5.5% of the 3 H (12.32 y) decays per year, the tritium in stored weapons must be replenished by irradiation of 6 Li in rods containing lithium in a reactor [reaction (14-12)] or produced in an accelerator. The reactor route using commercial LWR power reactors has been chosen in the United States. Lithium-containing absorber rods are to be irradiated with neutrons at nuclear power plants operated by the Tennessee Valley Authority and shipped to a new processing plant at the Savannah River site.

14.11.2 Production After the initial mining and milling of uranium ore, the uranium is leached 45 from the ore, (e.g. with nitric   acid), puri®ed by solvent extraction from uranyl nitrate UO2 …NO3 †2 solution, converted to UO3 , reduced to UO2 with hydrogen, converted to UF4 by the reaction of UO2 with hydrogen ¯uoride, and ®nally oxidized to UF6 with ¯uorine. Uranium hexa¯uoride has a vapor pressure of 1 atm at 56.48C and is suitable for increasing the 235 U 44

A one-kiloton nuclear explosive has an explosive energy output of 4184  109 kJ. Radon-222 is released from the ore when the uranium is extracted and from the radiumcontaining waste that is generated. 45

628

14.11 NUCLEAR WEAPONS

content above that in natural uranium by gaseous diffusion or centrifugation or magnetic separation.46 In the gaseous diffusion method of isotope separation, which is based on the kinetic theory of gases, the UF6 diffuses through porous barriers. The theoretical separation factor is 1.0043, but in practice it is closer to 1.003. Over a thousand stages are required to increase the 235 U content from 0.72% to about 93% in highly enriched uranium (HEU). The depleted uranium (DU) that remains contains 0.2 w% or less 235 U. Enrichment utilizing a gas centrifuge is more energy ef®cient. The 235 UF6 migrates toward the axis of rotation, where the enriched product is removed, while the 238 UF6 migrates toward the outside of the centrifuge, where it is removed. Atomic vapor laser isotope separation (AVIS) has been studied in the United States and France. Another laser-based method, separation by laser excitation (SILEX), uses UF6 as the feed material. Although there should be negligible loss of radioactive material in enrichment processes, liquid waste is generated when the equipment is cleaned. Also, there can be leakage of UF6 at various points in the processing. A medical monitoring program has been established for people who have worked at gaseous diffusion plants. Next, the enriched uranium hexa¯uoride is converted to UF4 followed by reduction with calcium to uranium metal, fabrication of weapon components, and assembly of the weapons. Workers at gaseous diffusion enrichment plants that also produce the metal may have been exposed to levels of ionizing radiation and toxic chemicals (e.g., beryllium) above current limits. There have been instances in which the metallic dust has escaped from air ®lters and has been carried into the environment outside the plant site. Approximately 57  105 tonnes of depleted uranium as UF6 were produced in the United States weapons program.47 In metallic form (density of 1907 g= cm3 ), uranium is used for shielding in medical x-ray equipment and for making tank armor and conventional weapons (e.g., armor-piercing shells). In addition to the United States, nine other countries have developed such weapons. It is also used in the form of ballast and counterweights in civilian and military aircraft. When ingested, 238 U (447  109 y), an a-emitter with a speci®c activity of 124 MBq=kg …335 mCi=kg†, is generally considered to be a toxic heavy metal that is retained by bone and can cause kidney damage. Because metallic uranium is pyrophoric (ignites spontaneously) when ®nely divided, it can become airborne as smoke containing very ®ne particles of UO2 . 46 Large mass spectrometers called calutrons also were used for enrichment at Oak Ridge during World War II. They later became the source of separated stable isotopes. 47 After irradiation with neutrons to produce plutonium, the depleted uranium contains a small amount of a-emitting 236 U (2342  107 y), which can contaminate the DU when it is put through the enrichment process to recover the 235 U.

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External exposure to DU, with its very low speci®c activity, is not a radiation hazard. At the time of writing, inhalation of DU particles is not considered to present a risk of cancer arising from its being a source of ionizing radiation. The risk of cancer in organs of the body from DU, as a heavy metal, has not been ruled out. Extensive research on the health hazards of uranium has been carried out over the years. Additional research seems to be needed to settle the questions that have been raised about health effects such as leukemia for people exposed to DU during or after military operations in recent years. A complicating factor is that less is known about the health hazard of the traces of 236 U, 239 Pu, and 240 Pu that may be in the DU if its origin was irradiated uranium. See the additional reading at the end of the chapter for a report on an environmental assessment in Kosovo. For a weapon based on 239 Pu, the plutonium is made according to reaction (13-44) by irradiation of 238 U in a nuclear production reactor. After irradiation, the fuel rods are chopped; the fuel (UO2 ) is dissolved in acid (e.g., nitric acid), and the plutonium and uranium are chemically coseparated (e.g., by solvent extraction) from the ®ssion products formed during the irradiation. The weapons-grade plutonium is chemically separated from the uranium, puri®ed, converted to plutonium metal, fabricated into the required components, and assembled into weapons. This reprocessing of the irradiated uranium generates large quantities of liquid radioactive waste. It also releases volatile ®ssion products. At the Hanford Reservation, for example, about 15 PBq (400,000 Ci) of 131 I (8.020 d) was released into the atmosphere between 1944 and 1947. The reactors used to produce the plutonium were cooled with water from the Columbia River until 1971. Radioactivated corrosion products [e.g., 60 Co (5.271 y) ] and any ®ssion products that escaped from the rods containing irradiated uranium contaminated the water that was returned to the river. If a weapon contains tritium, there are the additional steps of removing the tritium from the irradiated target, purifying it, and fabricating a weapon component. Because metallic plutonium, like metallic uranium, is pyrophoric, machining and other operations must be done with the ®re hazard in mind. There have been cases of spontaneous combustion. The oxide smoke of the a-emitting 239 Pu is a major radiological (inhalation) hazard. Until 1984 the government facilities located in some 32 U.S. states that produced nuclear materials and nuclear weapons were not required to operate in compliance with the applicable environmental laws and regulations that applied to commercial facilities such as nuclear power plants, factories, hospitals, and laboratories using or producing radioactive materials.48 Weapons 48

Environmental Restoration and Waste Management Program, U.S. Department of Energy, DOE=EM-001P (revised December 1992).

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14.11 NUCLEAR WEAPONS

facilities of all types operated as they had during the Manhattan Project, with the urgency and secrecy that was part of wartime weapons production. The nuclear weapons programs that ¯ourished in the United States and the Soviet Union during the Cold War have left a legacy of environmental problems that include the following.
Determination of health effects for workers in the weapons facilities and possibly for people living in the vicinity of the facilities
Site assessment and selection of remedial method49
Disposal of radioactive waste (Section 14.12) and nonradioactive toxic chemical waste stored at the facilities
Disposal or storage of weapons-grade 235 U and 239 Pu
Implementation of remedial action for facilities where groundwater has been contaminated by any hazardous substances
Decontamination of the facilities with respect to hazardous chemical substances and radioactive materials
Decontamination of the area around some of the facilities
Decommissioning of the facilities to make them available for other use

14.11.3 Testing Testing of nuclear weapons, especially atmospheric testing, has added to the radioactivity of the environment. At least 2419 tests have been carried out since 1945, and of these, 543 were atmospheric tests. In 1963 a Limited Test Ban Treaty banning nuclear tests in the atmosphere, in outer space, and under water was signed by the United States, the United Kingdom, and the Soviet Union. Testing continued, but the explosions were carried out underground with a limit of 150 kilotons under the 1974 Threshold Test Ban Treaty. The last such test in the United States occurred in September 1992. In September 1996, 158 members of the United Nations signed the Comprehensive Test Ban Treaty (CTBT), which bans all testing. This treaty was signed by the ®ve declared nuclear nations (``the Nuclear Club''), namely, China, France, Russia, the United Kingdom, and the United States. As of July 2001, 161 nations had signed the treaty and 77 had rati®ed it. The latter number includes only 31 of the 44 nations that have nuclear capability (i.e., possess nuclear reactors or conduct nuclear research). The treaty cannot go into effect, however, until it has been rati®ed by all the nuclear-capable nations. Ironically, experimental veri®cation of the treaty (a signed agreement) is a critical aspect of the CTBT, and doubts about veri®cation have delayed rati®cation. A network of over 300 stations equipped with sensors will be used 49

A site may be suitable for a nonnuclear use, or it may be converted into a safe storage facility. Existing facilities may be entombed or may be completely dismantled.

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for four types of monitoring: seismological, radionuclide, hydroacoustic, and infrasound [ (sound waves with inaudible frequencies below 20 Hz) for atmospheric testing]. Nuclear weapons testing (underground) by the declared nuclear powers ended after announced tests by France and China in 1996. The world was taken by surprise when India conducted three unannounced, simultaneous, underground tests on May 11, 1998, and two more on May 13. The tests involved both ®ssion and thermonuclear devices. India had previously detonated a ``peaceful nuclear explosive'' in 1974. A little over two weeks later, on May 28, Pakistan conducted ®ve underground tests. A sixth device was detonated on May 30. Thus, India and Pakistan moved from the group of probable (undeclared) nuclear nations to the group of declared nuclear nations.

14.11.4 Fallout and Rainout The extent to which the ®ssion products and residual ®ssionable material are deposited in the immediate area following detonation of a nuclear weapon in the atmosphere depends on the altitude at which detonation occurs and the type of weapon. The local effects of a large (kilotons to megatons) weapon detonated at an altitude of tens of thousands of feet are mainly those from the shock wave, from heat, and from irradiation by neutrons and g rays. Weapons of a megaton or larger generally release most of the radioactive debris (atomic vapor) in the stratosphere, where it is dispersed and distributed worldwide. The long-lived components have a residence time in the stratosphere of one to ®ve years, with an average of about two years. After the debris falls into the troposphere, it can reach the earth slowly as fallout of very ®ne particles, or it can be concentrated and carried to the earth's surface by rain (as rainout) or snow. Although most of the fallout and rainout from atmospheric tests was expected to accumulate relatively near the test site, in some incidences the ®ssion product cloud remained concentrated and traveled great distances before being brought to earth in rain. For example, after the Simon test, in Nevada on April 25, 1953, the highest fallout (rainout) recorded in the United States was in the region around Troy, New York. The weapons debris reached Troy in a jet stream 36 hours after the detonation and was deposited in a localized, exceedingly violent and destructive thunderstorm.50 In the case of detonations at or close to the earth, the bomb debris is adsorbed on soil, vegetable matter, and so on, which is carried upward as 50 See M. Eisenbud and T. Gesell, Environmental Radioactivity (From Natural, Industrial, and Military Sources), 4th ed., Academic Press, San Diego, CA, 1997, p. 292, and H.M. Clark, Science, ++ ",#, 619 (1954).

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14.11 NUCLEAR WEAPONS

large particles and settles out in a matter of minutes. The fallout is deposited locally and includes radioactivity induced by neutron capture reactions in the soil (or seawater if the detonation is over an ocean). When nuclear weapons are tested by underground detonations, most of the radioactivity remains underground, but there may be venting (tritium, noble gases, and other volatile ®ssion products) and localized fallout. Such tests can be detected seismographically and have provided information about the inner regions of the earth. Five weapons-produced ®ssion products, namely, 90 Sr (28.78 y) and its daughter 90 Y (2.67 d), 131 I (8.0207 d), and 137 Cs (30.07 y) and its daughter 137m Ba (2.552 m) are particularly hazardous when ingested (Section 14.13). More recently, 99 Tc (213  105 y) and 129 I (157  107 y) have also been receiving attention as long-term, internal radiological health hazards. Most of the ®ssion products from atmospheric weapons tests at the Nevada test site were released between 1952 and 1957. Beginning in 1983 and ending with a report in 1997, the National Cancer Institute (NCI) conducted a very challenging study to estimate the exposure to 131 I of the American people and to assess thyroid doses received by individuals across the country (3100 counties) from the Nevada tests.51 The report contains maps showing the activities of 131 I deposited on the ground and dose estimates for all counties. A third part of the 131 I fallout study, namely, assessment of the risk for thyroid cancer from the estimated exposures, was completed by the Institute of Medicine (IOM).52 Two conclusions in the IOM report are ``®rst, that some people (who cannot be easily identi®ed) were likely exposed to suf®cient iodine-131 to raise their risk of cancer and, second, that there is no evidence that programs to screen for thyroid cancer are bene®cial in detecting disease at a stage that would allow more effective treatment.'' The potential climatic effects of nuclear warfare were discussed in Chapter 3, Section 3.3.4.

14.11.5 Proliferation As more and more nations built nuclear power plants, the Soviet Union, the United Kingdom, and the United States became concerned that the plutonium in the irradiated fuel in these plants could be used to proliferate nuclear weapons. In 1970 the worldwide Nuclear Non-Proliferation Treaty (NPT) 51

Estimated Exposures and Thyroid Doses Received by the American People from I-131 in Fallout Following Nevada Atmospheric Nuclear Bomb Tests, National Cancer Institute, U.S. Department of Health and Human Services, October 1997. 52 Exposure of the American People to Iodine-131 from Nevada Nuclear-Bomb Tests: Review of the National Cancer Institute Report and Public Health Implications, Institute of Medicine, National Academy of Sciences, Washington, DC, 1998.

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that had been signed by 82 nations during the preceding two years went into effect for a period of 25 years. Under this treaty a signatory nation agreed that in exchange for having access to the technology for peaceful uses of nuclear energy (i.e., generation of electricity) it would not develop nuclear weapons and would not assist other nations to develop such weapons. It further agreed to accept international safeguards that include monitoring of the acquisition, storage, transfer, and use of all ®ssionable materials and sources of such materials. Safeguards inspections are carried out by the International Atomic Energy Agency. In 1995, when the NPT was renewed for an inde®nite period, there were over 162 signatories. Although the goal of the NPT is to prevent the spread of nuclear weapons, it also can be seen as protecting the environment from widespread radioactive contamination. The type of proliferation just discussed is sometimes referred to as ``horizontal proliferation.'' During the Cold War, the declared nuclear nations increased their stockpiles of nuclear weapons. This increase in number of weapons possessed by each nation is called ``vertical proliferation.'' A modern thermonuclear warhead is a complex system containing 235 U, 238 U, 239 Pu, Be, Li, 3 H, and 2 H as nuclear components. The uranium enrichment path to a weapon has a lower radiological health risk and may be more dif®cult to detect than the plutonium path, which requires chemical processing of the irradiated fuel with likely escape into the environment of detectable radioactive ®ssion products. In one type of thermonuclear explosive the thermonuclear reactants, 2 H and 3 H, are enclosed within the ®ssile material, which compresses and ignites the fusion reaction. In a second type, the ®ssile material and the mixture of hydrogen isotopes are in separate compartments. Radiation from the ®ssion reaction compresses the hydrogen mixture and ignites the thermonuclear reaction. Various proposed schemes for preventing the proliferation of nuclear weapons by nations that have not signed the NPT have been studied and evaluated.53 The general conclusion of the studies was that steps could be taken to make diversion of plutonium and enrichment of uranium more costly, more dangerous, and more time-consuming, but that there is no technical ®x (including using the 233 U 232 Th fuel cycle) to prevent proliferation. At best, a degree of proliferation resistance could be created.54 Also, it was concluded that fuel cycles involving reprocessing to remove the plutonium are more vulnerable than the once-through cycles in which the irradiated fuel is placed in a repository for long-term storage. 53

Two in-depth studies were the International Fuel Cycle Evaluation (INFCE) and the Nonproliferation Alternative Systems Program (NASAP). The latter, which began in 1976, was a program of the U.S. Department of Energy and was in support of INFCE. 54 For example, addition of ®ssion products would provide a measure of deterrence. However, no matter what is done to the fuel before irradiation or what is done when the fuel is reprocessed, the plutonium can be recovered by chemical separation.

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14.11 NUCLEAR WEAPONS

Prevention of the proliferation of nuclear weapons is dependent on nuclear safeguards, the measures that are taken to guard against the diversion of nuclear material from uses allowed by law or by treaty and to detect diversion or provide evidence that diversion has not occurred. The measures include physical security, material control (controlling access to and movement of nuclear material), and material accountancy. When India and Pakistan increased the proliferation of nuclear weapons in May 1998, they followed different production routes. India used plutonium separated from irradiated nuclear reactor fuel. Tritium needed for the thermonuclear explosive was produced at a facility in India. Pakistan used highly enriched uranium obtained by the centrifuge separation process. However, Pakistan also has nuclear reactors and a facility for reprocessing irradiated fuel to separate plutonium. Even though the end of the Cold War eliminated the need for large arsenals of nuclear weapons, the potential for diversion of ®ssionable material from nuclear power plants continues, and there is the added potential for theft of existing weapons or their components. Furthermore, the focus of nuclear deterrence moved to the ``rogue states'' and terrorist groups that might use nuclear or other weapons.

14.11.6 A Cold War Heritage: Weapons-Grade Plutonium and Weapons-Grade Uranium When the Cold War ended, one of the obvious questions that arose was, What should be done with the surplus plutonium and HEU that have been produced in the weapons program? The risk of theft caused nations with these materials to examine and strengthen their safeguards programs. On paper, there are several long-term options available for disposal of each of the two ®ssile materials. An argument for not converting both the plutonium and the HEU into waste is that they represent two stockpiles (``treasures'') of an energy source that were produced at great expense and have potential use as fuel in nuclear power plants in the future. For HEU (about 93% 235 U), an obvious long-term solution for dealing with the surplus is to simply convert the metal to UO2 and dilute the oxide with natural or depleted uranium oxide to obtain LEU (3±4% 235 U) for use as fuel for existing LWRs or for new LWRs in other countries. This dilution procedure is now well established and is being used. Since the material is no longer of interest for making a weapon after dilution below 20%, it can be stored. Among the objections to this dilution procedure is that plutonium will be produced from the 238 U in the LEU. However, because the plutonium will be sealed in irradiated fuel rods along with a large quantity of ®ssion products, it is considered to be in a ``theft-resistant'' state.

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The stewardship of the surplus weapons-grade plutonium is a much greater challenge than that for HEU. Isotope dilution is not an option. The estimated total amount of weapons plutonium in the world is 270 tonnes (metric tons). Perhaps about 200 tonnes will become surplus. Over 30 methods for guarding against use to make a nuclear explosive have been suggested. Five of these are as follows. 1. Store it as the metal in a criticality-safe manner and guard it for perpetuity for possible reuse in weapons or for future conversion to PuO2 and dilution of the oxide with natural or depleted uranium UO2 to obtain MOX that can be used in nuclear power reactors. 2. Convert it to MOX as soon as possible. 3. Treat it as waste by mixing it with ®ssion products and use known technologies to dispose of it after vitri®cation (incorporation in glass). 4. ``Destroy'' it in an accelerator-driven, subcritical ®ssion device in which the ®ssion energy would be recovered 5. Bury it underground in boreholes more than 4 km deep. Method 1 does not resolve the safeguards issue because a suitable, longterm storage facility does not exist, and 239 Pu …2410  104 y† decays into the longer-lived 235 U …704  108 y†. Method 2 requires that the existing commercial LWRs in the United States be modi®ed to use MOX as fuel. MOX is not a weapons material. It is being used in some of the European reactors. Method 3 reduces the energy value of the plutonium to zero, but requires a geological repository. The fourth method would require extensive development. In December 1996 the United States announced a decision to take a dualtrack approach using two of the four methods just listed: vitri®cation and conversion to MOX, for disposal of about 50 tonnes of surplus plutonium over a period of about 30 years. Approximately four years later Russia and the United States agreed that each country would dispose of 34 tonnes of plutonium, either as MOX to be used as fuel for civilian reactors or by mixing the plutonium with ®ssion product high-level waste and placing it in a waste repository.

14.12 RADIOACTIVE WASTE 14.12.1 Types and Sources In the United States, radioactive waste (radwaste) is usually classi®ed according to the following categories:55 55

Acronyms HLRW, ILRW, and LLRW, where R designates radioactive, are also used.

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14.12 RADIOACTIVE WASTE

High-level waste (HLW) Spent nuclear fuel (SNF) Transuranic waste (TRU) (waste containing elements beyond uranium in the periodic table) Low-level waste (LLW) Intermediate-level waste (ILW) (waste generated when water used to cool the core of a power reactor is decontaminated, and certain types of waste produced in reprocessing SNF) Mixed waste (MW) (HLW or TRU or LLW containing other hazardous materials such as PCBs, mercury, organic solvents, heavy metals and materials that are carcinogenic, toxic, ¯ammable corrosive, pyrophoric, or environmentally hazardous in some other way) Uranium mill tailings Contaminated soil Contaminated groundwater The disposal method used depends on the type of waste. Radioactive waste of the various types that are now in storage has been generated mainly in facilities used in the nuclear weapons program and in nuclear power plants. Additional waste has been generated in research reactors and in facilities such as those in hospitals, universities, and industry. New waste is being generated at all these facilities. For the weapons facilities, the new waste will result from decontamination of the equipment and buildings as the facilities are decommissioned. The same holds for commercial nuclear power plants that cease operation. Plants continuing to operate will, of course, continue to produce spent fuel and LLW. Normally, when a building (e.g., factory, apartment complex, etc.) is demolished, the debris includes concrete and scrap metal. The latter ®nds its way into the local metal supply. When a nuclear facility is decommissioned and leveled, both the concrete and the scrap metal may be radioactively contaminated, not simply on the surface where the unsafe areas are removable, but internally. Contaminated concrete is sent to a radwaste disposal site. Contaminated scrap metal, if detected, must not be recycled. Tens of thousands of tons of nickel and steel have been placed in storage for this reason. These metals may be of use in nuclear facilities. Safety standards for the transportation of nuclear waste are set at the international level by the International Atomic Energy Agency. Domestic regulations based on relevant parts of the IAEA standards are set by the Department of Transportation, as well as the NRC and the EPA. Packages and containers of various types are tested to withstand transportation accidents. For high-level waste and SNF, the appropriate local authorities are noti®ed of the route and schedule.

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14.12.2 Methods of Disposal Disposal is the process of isolating the waste from people and the environment. One criterion for a disposal site is location in an area of extremely low population density. A second criterion is that radionuclides in a permanent, underground disposal facility (e.g., a geological repository) not escape and contaminate the groundwater in the area for thousands of years. Predictions of how a repository will behave over extended periods of time are based on mathematical models that take into account the likelihood of catastrophic phenomena such as ¯oods, earthquakes, and volcanism. In addition, the models provide predictions on how any radionuclides that enter the groundwater will be transported (e.g., as simple ions, as ions bound to complexing agents,56 or depending on the pH, as colloids consisting of ions adsorbed on hydrous oxides such as those of iron and aluminum). Despite the advances that have been made in chemistry to date, relatively little is known about the fundamental chemistry relevant to the migration of the elements on the earth's surface and below the surface. This area of research provides both a challenge and an opportunity. It includes investigation of the solubilities, complexation, redox reactions, colloid formation, and sorption and desorption mechanisms of the ®ssion products and the actinide elements. In addition, there is need to develop more effective technologies that are both innovative and cost-effective to separate and convert hazardous wastes of all types into stable disposable forms. An additional requirement for a long-term radwaste disposal site is that it be intrusion-proof. For a geological repository, ``intrusion'' could mean mining for plutonium or mining to reach mineral deposits in the area. 14.12.2.1 High-Level Waste (HLW) and Spent Nuclear Fuel (SNF)

HLW includes the mixture of ®ssion products separated from irradiated reactor fuel when the fuel is reprocessed (for the nuclear weapons production) and often includes SNF that is stored without reprocessing. Transportation of HLW to sites for storage, predisposal treatment, and permanent disposal is a very important part of the management of such waste. Casks used to transport HLW by truck or rail are especially designed to provide radiation shielding and to remain intact in the event of an accident. The two major sources of HLW considered here are nuclear power reactors and facilities at which irradiated fuel and SNF have been reprocessed to remove the plutonium and recover 235 U. For an LWR with a burnup of 33 GWd=MTHM and annual removal of the third of the fuel having the highest burnup, each MTHM of SNF would 56

Complexing agents would include EDTA used as a decontaminating agent or naturally occurring substances such as humic and fulvic acids.

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300

A: < 1 minute B: 1 minute to 1 hour C: 1 hour to 1 day D: 1 day to 1 year E: > 1 year

250

Number

200 150 100 50 0

A

B

C Group

D

E

FIGURE 14-13 Distribution of ®ssion products in spent LWR fuel according to half-life in speci®ed time ranges.

contain about 35 kg of ®ssion products and about 10 kg of transuranic elements (Np, Pu, Am, and Cm), of which about 9 kg would be plutonium.57 The radioactivity of the ®ssion products and that of the actinides at the time when the reactor is shut down decreases rapidly at ®rst because of the high proportion of short-lived radionuclides. Figure 14-13 illustrates the half-life distribution for ®ssion products in the SNF when it is removed from the reactor. As spent nuclear fuel is stored, the ®ssion product radioactivity will be determined increasingly by the radionuclides with long half-lives.58 Fission products in the SNF having a half-life greater than one year are listed in Table 14-11. The four long-lived ®ssion products that require long-term storage in a repository are 90 Sr (28.78 y), 99 Tc (213  105 y), 129 I (157  107 y), and 137 Cs (30.07 y). 57 By the year 2008, burnup for LWRs in the United States is expected to increase to about 39 GWd=MTHM for BWRs and about 50 GWd=MTHM for PWRs. The concentrations of ®ssion products and transuranic elements in the SNF will, therefore, increase. 58 In an operating reactor, the short-lived ®ssion products that are daughters of longer-lived ®ssion products reach transient or secular equilibrium concentrations. Note that the short-lived daughters are counted according to their own half-lives in Figure 14-13, even though they decay with the half-life of the parent. As a good approximation, ®ssion products with very long half-lives initially accumulate linearly with time.

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TABLE 14-11 Fission Products and Actinides with Half-Life Greater than 1 Year That Are in LWR Spent Fuel Fission productsa Radionuclide 3

H Kr 90 Sr 90 Y* 93 Zr 99 Tc 106 Ru 106 Rh* 107 Pd 121m Sn 125 Sb 125 Te* 126 Sn 126m Sb* 126 Sb* 129 I 134 Cs 135 Cs 137 Cs 137m Ba* 147 Pm 151 Sm 154 Eu 155 Eu 85

Half-life 12.32 y 10.76 y 28.78 y 2.67 d 15  106 y 213  105 y 1.020 y 29.9 s 65  106 y  55 y 2.758 y 58 d 25  105 y 19.90 m 12.4 d 157  107 y 2.065 y 23  106 y 30.07 y 2.552 m 2.6234 y 90 y 8.593 y 4.75 y

Actinidesa Radionuclide 234

U U 236 U 238 U 237 Np 236 Pu 238 Pu 239 Pu 240 Pu 241 Pu 242 Pu 241 Am 242m Am 242 Am* 243 Am 243 Cm 244 Cm 245 Cm 246 Cm 235

Half-life 246  105 y 704  108 y 2342  107 y 447  109 y 214  106 y 2.87 y 87.7 y 2410  104 y 656  103 y 14.4 y 375  105 y 432.7 y 141 y 16.02 h 737  103 y 29.1 y 18.1 y 85  103 y 476  103 y

a

Includes short-lived radioactive daughter (asterisk = *) present with the preceding long-lived parent.

The actinide radionuclides, including transuranic nuclides, having a half-life greater than one year that are contained in the fuel are also listed in Table 14-11. If SNF is reprocessed, the small amount of uranium and plutonium that is not recovered (perhaps 0.1±0.5% by weight) and the other TRU elements remain with the ®ssion products in the HLW waste. After 10 years of decay, the contribution of ®ssion products to the long-term heat release consists of about 43% from 90 Sr 90 Y and about 49% from 137 Cs 137m Ba. The isotopes of plutonium, americium, and curium contribute 52, 29, and 19%, respectively, of the heat released from actinides after 10 years. When the nuclear power industry was established in the United States, it was intended that the spent nuclear fuel would be reprocessed after being

640

14.12 RADIOACTIVE WASTE

stored for a ``cooling'' time of about 150 days under water in pools located at the power plant site. During the cooling time, the decay heat would be removed from the short-lived ®ssion products. There are several reprocessing schemes for recovering the residual 235 U and 238 U and separating the reactorgrade 239 Pu (with higher concentrations Pu isotopes) from the ®ssion products and then separating the uranium and plutonium. One such scheme was described in Section 14.11.2 for separating weapons-grade Pu. Reprocessing of spent fuel from commercial nuclear power plants was banned in the United States in 1976 because of concern about the possible proliferation of Pu-based nuclear weapons. After the ban went into effect, the spent nuclear fuel became part of the once-through fuel cycle (i.e., from reactor to a repository for permanent disposal as waste).59 In 1982 (Nuclear Waste Policy Act) the U.S. Department of Energy agreed to begin accepting commercial SNF for storage or disposal by January 31, 1998. The electric utilities have been contributing to a Nuclear Waste Fund to pay for construction of a storage or disposal facility (repository). The Yucca Mountain geological storage facility (described shortly) will not be available until 2020 at the earliest. As the storage pools for SNF became ®lled to capacity, some nuclear power plants built heavily shielded, above ground, dry, secure storage facilities to hold the older spent fuel. These facilities are passively air-cooled. Unfortunately, reliance on on-site, dry storage nuclear power plants keeps the SNF distributed about the country. Thus, spent fuel is stored in 35 states rather than in a single, isolated geological repository. The projected annual rate of SNF discharge in the United States is about 1900 MTHM until the year 2014. In the year 2000, the total amount of spent fuel stored in various places amounted to 40,446 MTHM. If no new nuclear power plants are built, the rate of increase in spent fuel will drop to zero at a rate that depends on how many plants have their operating licenses extended (e.g., by 20 years) beyond the original period of 40 years. Projections for cumulative discharges of spent nuclear fuel worldwide were made beginning with the year 1993 (when data for eastern Europe became available). According to one projection,60 the annual discharge rate will decrease from 8513 MTHM in 2000 to 8179 MTHM in 2010. This change during the decade may be too small, since the increase in nuclear power generation in a country such as Japan may be more than offset by the rate of decrease resulting from the closing of nuclear power plants in countries that have a politically based nuclear power moratorium. In 2000, spent nuclear fuel was being generated in about 490 nuclear power plants in 33 nations. Not all of the spent fuel was being stored. Reprocessing is carried out in France, Japan, 59 Although commercial reprocessing of spent fuel became legal again in the United States in 1980, it is not economically attractive for a number of reasons. 60 Nuclear Energy Data 2000, Nuclear Energy Agency, OECD, Annapolis Junction, MD 20701.

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641

Russia, and the United Kingdom. Some of these nations reprocess spent fuel shipped from other nations. Russia has indicated an interest in expanding the past practice of importing and storing nuclear waste (e.g., spent fuel) for a fee. Western Europe and Asia would be the source of the spent fuel, which would eventually be reprocessed. Predisposal treatment of HLW that has been generated by reprocessing irradiated fuel in the weapons program in the United States for over 50 years presents a more dif®cult challenge. Most of the HLW is liquid (aqueous) waste that contains inorganic salts, organic solvents, complexing agents such as ethylenediaminetetraacetic acid, nonvolatile ®ssion products, and small amounts of uranium, plutonium, and other transuranic elements.61 At the Hanford Reservation, where plutonium was produced during the Manhattan Project and in subsequent years, the waste was stored in 177 large underground tanks having provisions for removing decay heat. Some tanks have vented gases (e.g., hydrogen), produced by radiolysis of water, and exothermic reactions involving nitrates have occurred in the stored waste. Most of the tanks (149) were single-wall tanks that were state-of-the-art vessels when built during World War II. HLW (about 140,000 gallons by 1996) had leaked from about 67 of these tanks. Transfer of liquid HLW from the old tanks to new, million-gallon, double-walled tanks (Figure 14-14) has been ongoing for several years. Liquid HLW stored in tanks for a long time tends to separate into a strati®ed mixture of a supernatant solution, a salt cake consisting of compounds such as carbonates, phosphates, sulfates, and nitrates, and a sludge containing most of the radioactivity. After liquids have been removed to reduce the volume of the waste, the solid can be calcined to a granular solid to reduce its leachability, or the waste can be vitri®ed with a borosilicate glass having a low solubility in water.62 Vitri®cation (at temperatures above 10008C) reduces the volume of high-level liquid waste by about 75%. An additional ``engineered barrier'' to prevent escape of radionuclides from a repository into the environment (if water enters the repository) is introduced by sealing the glass ``logs'' in stainless steel canisters (3.0 m  0.6 m). Locations that have been proposed for permanent disposal of HLW include deep stable geological repositories, stable deep sea sediments consisting of clay and located in international waters, and outer space.63 In the past, ocean disposal of various types of radioactive waste has been used by several nations. 61 Strontium-90 and 137 Cs have been extracted from some of the waste for use in intense sources of ionizing radiation. 62 Vitri®cation of HLW has been under development for about 40 years. It has been employed since 1978 in Europe, where there are at least three vitri®cation facilities. Such facilities began operation in the United States in 1997. 63 Temporary disposal in outer space is a de facto method in the sense that there are nuclearreactor-powered satellites parked in space.

642

14.12 RADIOACTIVE WASTE

Filtered air intake Leak detection pit

Liquid level gauge Ground level

Filtered air exhaust

Primary tank Secondary tank

Liquid

Reinforced concrete Sludge

Carbon steel

Annular space for leak detection

FIGURE 14-14 Double-shell tanks with improved leak detection systems and waste containment features built to replace the old single-shell tanks. From Restoration and Waste Management (EM) Program. An Introduction, U.S. Department of Energy. DOE=EM-0013P (revised December 1992).

Radwaste [estimated total of about 35 PBq (0.95 MCi) ], including plutonium, from the Sella®eld reprocessing plant in the United Kingdom has been dumped into the North Sea. The United States disposed of one submarine reactor, that of the Seawolf (see footnote 36), and lost two nuclear-powered submarines at sea. It also dumped sealed containers of radwaste into the Paci®c Ocean about 50 miles from the coast of California, for an estimated total of about 3.5 PBq (95 kCi). The former Soviet Union disposed of 16 cores of reactors from submarines along with other containers of radioactive waste near the Novaya Zemlya archipelago in the Barents Sea. Additional waste was dumped into the Sea of Japan and the Kara Sea, so that the estimated total was about 93 PBq (2.5 MCi). At least 12 other countries are known to have used ocean disposal of radwaste in estimated amounts up to megacuries. Although ocean dumping of radioactive waste is now prohibited by international law, disposal of radwaste at sea is still proposed. In the subseabed method, the waste would be placed in sealed canisters, which would be lowered into holes drilled hundreds of meters into the seabed of deep oceans. The canisters in a given hole would be separated by a layers of added sea sediment. Finally, the top section of the hole would be permanently sealed with sediment.

14. THE NUCLEAR ENVIRONMENT

643

In the 1950s the USSR began to inject liquid HLW into the earth, 300 m or more below the surface, near the sites of three nuclear weapons facilities (Krasnoyarsk-26, Mayak, and Tomsk-7), where irradiated uranium was reprocessed to recover the plutonium. Some 55 EBq (1.5 GCi) of waste, mostly 90 Sr and 137 Cs, was disposed of in this manner. At Mayak, where plutonium was produced and the irradiated uranium was processed, liquid waste was released into the Techa River, which ¯ows into a storage facility: Lake Karachai. In the United States, a total of about 60 PBq (1.6 MCi) was injected underground or released into streams, soil, seepage basins, or ponds at the Oak Ridge, Savannah River, and Hanford facilities. LLW was injected into the ground at Hanford WA brie¯y at the beginning of the nuclear weapons program, and radwaste mixed with concrete was injected into shale formations for several years at the Oak Ridge nuclear facility. About 60 PBq of waste was injected underground or released into streams, soil, seepage basins, or ponds at Oak Ridge, Savannah River, and Hanford. In the mid-1990s the strategy for disposal of HLW in the United States included construction of a temporary, above ground, monitored retrievable storage (MRS) facility, where spent nuclear fuel and other HLW would be stored, loaded into canisters, and eventually loaded into shipping casks for transfer to a repository. Dif®culties in locating a politically acceptable site and fear that interim storage might delay construction of a repository left the future of an MRS in doubt, but did not rule out establishing several smaller interim storage sites. Deep geological disposal of HLW and has been chosen by many countries, including Canada, Finland, France, Germany, Japan, Spain, Sweden, Switzerland and the United States. In the United States, the Committee on Separations Technology and Transmutation Systems of the National Research Council examined the various methods of radioactive waste disposal and concluded the following, with respect to the health and safety issues for the disposal of nuclear waste: ``For disposal, the lowest to highest risk alternatives appear to beÐgeologic repositoryÐsurface.'' (See Additional Reading and Sources of Information, Nuclear Wastes 1996.) The rock formation surrounding the storage rooms serves as the natural and the main barrier against escape of the radioactive material into the environment. Most countries construct or plan to construct an experimental facility as a learning experience before selecting and developing a ®nal repository site. A popular completion date is the year 2020. A potential site for a repository in the United States is Yucca Mountain, Nevada, which is roughly 160 km (100 miles) northwest of Las Vegas. This site (Figure 14-15), which consists of volcanic tuff, has been undergoing characterization for several years. Work on the site began in the 1950s. A

644

14.12 RADIOACTIVE WASTE

FIGURE 14-15 Yucca Mountain, Nevada, candidate site for the ®rst U.S. geologic repository. From Managing the Nation's Nuclear Waste, DOE=RW-0263P, U.S. Department of Energy, 1990.

few characterization projects include studies of redox reactions, radionuclide retention, hydrochemistry, and groundwater degassing. The Yucca Mountain facility was initially scheduled to begin receiving 30,000 tonnes of spent fuel from commercial nuclear power plants and other HLW (defense waste, as glass cylinders in canisters), by January 31, 1998. Opponents of the use of this site point out that it is located in the state that is third, after California and Alaska, in frequency of earthquakes and that the mountain is within 70 km of several volcanoes. In addition, there is at least one fault within the mountain. For these reasons and others concerning the water table, the opponents argue that it is dif®cult to show that the HLW would remain undisturbed for the required 10,000 years. If the site is approved by the Environmental Protection Agency, disposal of about 70,000 tonnes of SNF (the design limit) and other HLW in rooms 300 m below the surface would begin in the year 2010 and proceed as shown in Figure 14-16. At a disposal rate of about 3000 metric tons of spent fuel per year, the design limit would be reached in 2033. Closure could be between 50 and 300 years after the ®rst waste is accepted.

645

14. THE NUCLEAR ENVIRONMENT

Civilian reactor sites

SNF

acce

pted

cepted

HLW ac

HLW

SNF

High-level waste production and storage sites

Ra

Ra

m

p

mp

Geological repository

FIGURE 14-16 Civilian radioactive waste management system for spent nuclear fuel (SNF) and high-level waste (HLW). From U.S. Department of Energy, Of®ce of Civilian Radioactive Waste Management, Report DOE=RW-0473.

Transmutation of long-lived ®ssion products in HLW into shorter-lived radionuclides or even stable nuclides also has been proposed many times as a method for making HLW less radiotoxic and reducing the amount of HLW requiring storage in a geological repository. One technique, accelerator transmutation of waste (ATW), uses an accelerator rather than a dedicated reactor to change the isotopic composition of HLW. An example of the transmutation of the long-lived ®ssion product 129 I (157  107 y) by successive neutron capture and negatron decay is 129

I ‡ 1n ! 131

130

I …1236 h† b ‡

Xe…s† ‡ 1n !

132

130

Xe…s†

Xe…s† ‡ 1n !

646

14.12 RADIOACTIVE WASTE

14.12.2.2 Transuranic (TRU) Waste

TRU waste contains a-emitting transuranic elements (Z > 92) with half-lives greater than 30 years and concentrations greater than 100 nCi per gram of waste. This category of radioactive waste consists mainly of paper, clothing, equipment, tools, and soil contaminated with plutonium; plutoniumcontaining liquid waste generated in decontaminating glassware, and so on; dust and chips of metallic plutonium used for weapons production; plutonium dioxide; and any other materials that may have been contaminated with plutonium or other transuranic elements. Perhaps 2% of the TRU waste requires remote handling. A facility known as WIPP (Waste Isolation Pilot Plant) has been constructed for geological waste disposal of the TRU waste that has been generated in the weapons program. The waste must be stored in barrels, and there is a maximum allowable concentration of Pu that cannot be exceeded. WIPP (Figure 14-17), which includes facilities for research, is located in salt (rock salt, NaCl) deposits about 42 km (about 26 miles) east of Carlsbad, New Mexico. Salt beds or domes are considered to be suitable for geological disposal because large rooms can be built in the deposits without structural support. Also, salt has a relatively high thermal conductivity, is relatively impermeable to water,

Warehouse/shops Salt storage area Support building Waste handling building Exhaust shaft Waste shaft Salt handling shaft

Air intake shaft a l are enta m i r e Exp

a

l are

enta

erim Exp

Rock behavior area

Heated pillar Circular brine inflow test room

New Mexico

Transuranic waste storage area

FIGURE 14-17 Cross-sectional view of the Waste Isolation Pilot Plant in Eddy County, New Mexico. From Environmental Management 1995, U.S. Department of Energy, DOE=EM-0228, February 1995.

14. THE NUCLEAR ENVIRONMENT

647

and self-seals around voids so that the mined rooms, located 655 m (2150 ft) below the surface and containing the packaged waste, will eventually re®ll with salt and entomb the waste. The facility was completed in 1988 but was not opened on schedule because of structural, management, and legal problems, as well as political opposition and questions that were raised about the retrievability of waste that would be stored in the salt deposit during a trial period. Technical approval for use of WIPP was given by EPA in May 1998, and the site was opened in March 1999. The initial permit from the New Mexico Environmental Department was for nonmixed TRU waste. Later a permit was issued for mixed TRU waste. It has been estimated that WIPP will be ®lled to capacity (175, 600 m3 ) after about 35 years of operation and will be closed in about 2099. There are to be warning markers and barriers around the site. Salt domes have been explored for radwaste disposal in Germany. An example is the Gorleben dome in northern Germany. Interim waste storage facilities have also been built at Gorleben. 14.12.2.3 Low-Level Waste (LLW)

In the United Sates, low-level waste consists of a broad spectrum of radioactively contaminated material that does not qualify as HLW, SNF, TRU, or uranium mill tailings. Examples are contaminated clothing, gloves, shoes, tools, paper towels, pieces of equipment, ion exchange resin, and animal carcasses. Low-level waste is generated in nuclear power plants, governmentowned facilities, industrial and academic research laboratories, particle accelerator facilities, hospitals, and plants manufacturing radiopharmaceuticals or devices containing radioactive material. Less than 5% of the LLW requires the use of shielding during handling and transportation. It has generally been assumed that any LLW discharged (within legal limits) into public sewers by hospitals, laundries, and manufacturers is diluted to such a degree that it does not constitute a health hazard. Consistent with the known radiochemistry of radionuclides in very dilute aqueous solutions, however, certain radionuclides tend to reconcentrate on surfaces such as the particles of precipitates of hydrous oxides. For example, 60 Co (5.271 y) has been found in the sludge and ash produced in municipal waste treatment plants. Phytoremediation is a method for extracting radionuclides present at low concentration in soil and in aqueous solution. Sun¯ower plants, certain weeds, and willow trees, for example, have been shown to preferentially concentrate uranium, cesium, and strontium. If shown to be effective in a demonstration project, the method could be used on a large scale. Eventually the contaminated plants and trees would be incinerated to provide an ash containing the radionuclides at a higher concentration.

648

14.12 RADIOACTIVE WASTE

LLW is usually very bulky and, therefore, is also known as high-volume waste. The cost of disposal of LLW is determined by its volume; hence, there is a strong motivation to reduce the volume by compaction or incineration. LLW is generally disposed of in licensed, near-surface (shallow land) facilities. These facilities must be designed to afford protection from releases of radioactivity to the general population and to the individuals who operate the site, as well as to inadvertent intruders. The design also must ensure stability of the site after closure. Waste (in sealed containers) is placed in trenches which are eventually covered with soil and other materials to restrict the in¯ow of water. In the United States, the burden of disposing of all civilian LLW rests with the individual states. Groups of neighboring states can form regional compacts to share a disposal site if they can ®nd one that is politically acceptable. DOE has been disposing of LLW at the Nevada test site and at other major government sites that already have established LLW disposal facilities. Since 1983 LLW has been classi®ed further by the U.S. Nuclear Regulatory Commission. There are three classes, A, B, and C, based on the concentration of radionuclides and the length of time (< 100 y, 100 500 y, and > 500 y) required for the radioactive material to decay to a level such that an intruder would not receive a dose of more than 15 mrem=y. In the United Kingdom, investigation of the geology near the Sella®eld reprocessing facility was begun in 1997 for possible location of an underground repository for low-level and intermediate-level waste. 14.12.2.4 Mill Tailings

After acid leaching of the uranium ore, the residual sands contain 960±3700 Bq of 226 Ra (1599 y) and 2590±22.2 kBq of 230 Th (754  104 y) per kilogram (26±100 nCi of 226 Ra and 70±600 nCi of 230 Th per kilogram). These uranium mill tailings either are stabilized by a covering of soil and rock (Figure 14-18) or are removed for disposal at a more remote location on DOE-owned land and then covered. Figure 14-19 shows the location of most of the uranium mill tailings in the United States. The EPA standard for the limit of release of 222 Rn from tailings with a permanent radon barrier is 740 mBq m 2 s 1 (20 pCi m 2 s 1 ). Mill tailings that were used as ®ll around basements of buildings after World War II have been removed to a disposal site. Buildings that were signi®cantly contaminated have been razed.

14.12.3 The Cold War Mortgage The U.S. Department of Energy has referred to the environmental management problems associated with the facilities used for the production of nuclear

649

14. THE NUCLEAR ENVIRONMENT

Tailings pile (active) Tailings (liquid)

Earthen dam

Tailings from mill

Diversion channel

Tailings (saturated)

Tailings pile (reclaimed) Debris from the mill Rip rap

Earthen dam

Vegetation Radon barrier

Rock or rock/soil

Diversion channel

Tailings pile

FIGURE 14-18 Reclaiming the tailings pile from a uranium mill (rip rap is cobblestone or coarsely broken rock used for protection against erosion of embankment or gully). From Decommissioning of U.S. Uranium Production Facilities, U.S. Department of Energy, DOE=EIA-0592, February 1995.

weapons as the ``Cold War mortgage.''64 Another term is ``the environmental legacy of nuclear weapons research, production and testing and DOE funded nuclear energy and basic science in the United States.''65 Actually, problems such as disposal of stored liquid HLW began during the Manhattan Project in World War II and increased in magnitude during the Cold War.66 Of the three major weapons production sites, Hanford, Oak Ridge, and Savannah River, the Hanford site is expected to be the most dif®cult and costly to stabilize and remediate.67 Reprocessing irradiated uranium at this site to 64 Estimating the Cold War Mortgage, DOE=EM-0232, U.S. Department of Energy, Of®ce of Environmental Management, 1995 (updated annually). 65 Status Report on Paths to Closure, DOE=EM-0526, U.S. Department of Energy, Of®ce of Environmental Management, 2000. 66 The actual date when the ®rst Cold War ended is controversial. A commonly used range of dates is between 1989, when the Berlin Wall fell, and 1991, when the USSR ceased to exist. 67 Estimated dates for completion of remediation are as follows: Hanford, 2046; Savannah River, 2038; and Oak Ridge, 2014. Remediation of the site of the Idaho National Engineering and Environmental Laboratory, in Idaho Falls, is scheduled for completion in 2050.

650

14.12 RADIOACTIVE WASTE

Most uranium mill tailings are located in the western United States at the locations shown on the map. FIGURE 14-19 Locations of uranium mill tailings. From Radioactive Waste: Production, Storage, Disposal, U.S. Nuclear Regulatory Commission, NUREG=BR-0216, July 1996.

recover the plutonium over the period from 1944 to the early 1980s generated about 21  105 m3 …55  106 gal† of liquid, high-level radwaste with an activity of about 17 EBq (0.45 GCi). Also located at the Hanford Reservation are nine large reactors that were used to produce plutonium. It is likely that all or most of these will be buried on the site. For several of the weapons production sites, the groundwater is contaminated with both radioactive and nonradioactive hazardous materials that are likely to migrate beyond the site boundaries. As an example, the groundwater beneath about 388 km2 …150 mi2 † of the 1450 km2 …560 mi2 † Hanford Reservation is contaminated and is believed to be moving toward the Columbia River. The Idaho National Engineering Laboratory is another major site at which irradiated fuel (e.g., from the cores of nuclear submarine reactors) has been reprocessed and liquid HLW has been stored. Sections of hulls containing the reactors (minus the fuel) from decommissioned submarines are buried in disposal trenches at Hanford. At sites already mentioned, and at more than 100 additional sites, over 378  103 m3 …100  106 gal† of radioactive and mixed liquid waste are stored in over 300 tanks. In addition, there are about 3  106 m3 of buried radioactive or hazardous waste, about 250  106 m3 of contaminated soil, and over 23  109 m3 …600  109 gal† of contaminated groundwater.

14. THE NUCLEAR ENVIRONMENT

651

Despite the large volume of the HLW stored at DOE sites, the total radioactivity of these wastes is less than that of wastes stored as spent fuel from commercial nuclear power plants. During the Cold War period, two plants for commercial reprocessing of spent fuel from nuclear power plants were built. Only one of the plants, that at West Valley, New York, was put into operation. It was operated from 1966 to 1972, when it was shut down for modi®cations to increase its capacity. It never resumed operation. Liquid HLW and unreprocessed spent nuclear fuel remained stored on the site until about 1985, when DOE initiated decontamination of the site. A facility (a melter) for vitrifying HLW was built and operated successfully, a result that led to the building of a second facility at the Savannah River site.

14.13 PATHWAYS FOR INTERNAL EXPOSURE TO IONIZING RADIATION Unlike external exposure, which requires only that ionizing radiation from a source external to the body be absorbed in the body, the pathways for internal exposure can vary from direct injection of a radiopharmaceutical to a more complex pathway through the food chain. The human body has evolved in an environment containing naturally radioactive materials in the atmosphere, rocks, soil, lakes and oceans, drinking water, and foods of all types. The pathways from these components of the environment into the human body are rather obvious and are usually of little concern to a person in the course of routine daily life. If, however, human activity leads to a signi®cant increase in the concentration of radioactive material (naturally occurring or anthropogenic) in one or more of the many environmental components, questions about potential health hazards arise. Evaluation of the magnitude of a potential hazard requires an understanding of the chemistry of the material as it moves along an environmental pathway to a point where it may be ingested or inhaled by a human. The information needed to evaluate a potential hazard includes the following:
Identity and quantity of each radionuclide present in the environment and its key nuclear properties [half-life and type(s) of radiation emitted]
Environmental chemistry of the elements represented by the radionuclides (e.g., chemical processes such as chelation) that could increase or decrease the concentration of the radionuclides as they move along a particular pathway
Physiological chemistry of the elements including the biological half-life Tbiol as a measure of retention by the human body, distribution among the organs of the body, chemical reactions (e.g., complexation), and physical processes such as isotope dilution with a stable isotope that could accelerate elimination from the body

652

14.13 PATHWAYS FOR INTERNAL EXPOSURE TO IONIZING RADIATION


Biological concentration in plants and animals
Particular radiological health hazard(s) associated with each radionuclide
Identi®cation of any segment of the population that might be especially vulnerable Figure 14-20 is a simpli®ed ¯ow diagram that shows the major pathways by which radionuclides go from the atmosphere, surface water or groundwater, soil, and rocks into the human body. The major pathway for 226 Ra (1599 y) and 228 Ra (5.76 y) is the same as that for calcium, that is, through agricultural produce and milk. Water used for drinking and cooking can also be an unsuspected source of radium. Potassium 40 …127  109 y† enters the body through fruits and vegetables that are correctly recommended as very good sources of potassium. As discussed in Section 14.4.3.2, inhalation is the pathway into the body for 222 Rn and hazardous quantities of the two short-lived, a-emitting progeny of radon, 218 Po (3.10 m) and 214 Po (163.7 ms). Two relatively long-lived progeny of 222 Rn, the b emitter 210 Pb (22.6 y) and its a-emitting granddaughter 210 Po (138.38 d), also enter the body by inhalation as particulates contained in cigarette smoke. Polonium-210 has been implicated as a contributor to the carcinogenicity of cigarette smoke.

Atmosphere

Aquatic plants

W a t e r

Food crops Pasturage

Children men women

Sediment

Animals Meat

Aquatic animals

Milk and milk products

Feed crops

R o c k s a n d s o i l

FIGURE 14-20 Major pathways for the uptake by humans of radionuclides in the environment.

14. THE NUCLEAR ENVIRONMENT

653

Inhalation of ®ssion product radionuclides now in the atmosphere from past weapons tests is not considered to be a signi®cant source of exposure. However, inhalation of ®ssion products and possibly plutonium could have serious consequences for someone a few miles downwind of the explosion of a nuclear weapon, an explosion at a storage site for high-level waste, or a chemical explosion at a large nuclear reactor. The 17 radioisotopes of iodine that are produced in nuclear ®ssion and are released into the atmosphere by a nuclear explosion or a nuclear accident return to the earth as fallout or rainout. They can contaminate local water supplies, leafy vegetables, grass in pastures and, therefore, milk supplies, if it is the season when cows are in the pasture. Because iodine concentrates in the thyroid when it is ingested, most of the absorbed dose from ionizing radiation emitted by a radioisotope of iodine is localized in the thyroid. Except for 131 I (8.0207 d) and 129 I …157  107 y†, the radioisotopes of iodine are short-lived and will probably decay to a very low level before they become an ingestion hazard. Because of the relatively long biological half-life (138 d) of iodine, 131 I (Figure 13-10) can deliver a large dose of ionizing radiation …b , g† to the thyroid. Contaminated milk is the major pathway to the thyroid of children, who constitute the most vulnerable segment of the population because they drink a relatively large amount of milk and have relatively small thyroid glands (which leads to a higher radioiodine concentration than for an adult); moreover, since their thyroid glands are still growing, the cells are especially radiosensitive. Relative to 131 I, 129 I has a very low speci®c activity and is considered to be a less hazardous component of ``fresh'' fallout or rainout. However, if released into the environment, it accumulates and could constitute a potential hazard in the future. A compound such as KI, a ``thyroid blocking agent,'' containing the stable isotope 127 I can be administered in tablet form prior to the arrival of 131 I or other radioisotopes of iodine, if there is advance warning. The stable iodide taken up by the thyroid reduces the uptake of radioiodide. The ®ssion products 137 Cs (30.07 y) and 90 Sr (28.78 y) also leave the atmosphere and enter the food chain or the water supply as fallout or rainout. Either they immediately contaminate any leafy vegetables in the ®elds before they can be harvested or they contaminate the soil in farms and dairies and, therefore, later and for many years, contaminate crops grown in the soil for human and animal consumption. As a soil contaminant, 90 Sr will have the chemistry of Sr2‡ (i.e., similar to that of Ca2‡ ). The ions of both Sr and Ca will undergo cation exchange reactions. Strontium, therefore, being like calcium, is a bone-seeking element. If 90 Sr is ingested, the ionizing radiation (b ) from 90 Sr and its daughter, 90 Y, (2.67 d) (Figure 13-13) can cause bone tumors, bone cancer, and leukemia. Uptake of 90 Sr or 137 Cs, unlike that of 3 H and 14 C, is not reduced to a useful extent by

654

14.13 PATHWAYS FOR INTERNAL EXPOSURE TO IONIZING RADIATION

natural isotope dilution with stable isotopes in food. Lime (CaO) has been used to treat 90 Sr-contaminated soil to compete with and reduce the uptake of 90 Sr by vegetables. The main pathways for 137 Cs are from food grown in contaminated soil, from ®sh living in contaminated water, and from meat (e.g., that of sheep and reindeer). Fertilizers with high potassium content have been used to reduce the uptake of 137 Cs by plants from contaminated soil. When 137 Cs is ingested, it becomes rather widely distributed in muscle tissue. As expected, the chemistry of cesium is similar to that of potassium, but cesium passes more slowly through cell membranes. Oral administration of prussian blue, Fe4 Fe…CN6 † Š3 , has been used since the mid-1980s to accelerate the clearance of ingested 137 Cs from the body. Prussian blue has low toxicity and is not absorbed from the intestinal tract, where it acts as an ion exchanger for monovalent cations such as 137 Cs‡ but does not interfere with the serum levels of K‡ . This treatment has been found to reduce the biological half-life of 137 Cs (140 d) by a factor of 2±3. Prussian blue has been studied in laboratory animals and has been used to treat people and animals (as sources of meat) following the release of signi®cant amounts of 137 Cs in accidents. The actinide elements that have half-lives long enough to be of environmental concern are thorium, uranium, neptunium, plutonium, americium, and curium. A number of the isotopes of plutonium, americium, and curium (Table 14-11) are produced by multiple neutron capture reactions. Important oxidation states of these elements in the environment are Th(IV); U(IV), U(VI); Np(IV), Np(V); Pu(III), Pu(IV), Pu(V), Pu(VI); Am(III); and Cm(III). The extent to which these elements are mobile in soil and natural waters depends on a number of factors such as the degree of hydrolysis, the presence of adsorbents, and the presence of naturally occurring humic and fulvic acids (Chapter 9, Section 9.5.7), which can function as complexing agents and=or reducing agents. In the environment, plutonium [238 Pu (87.7 y), 239 Pu (2,410 y), 240 Pu (6560 y), and 241 Pu (14.4 y) and its daughter 241 Am (432.7 y) ] are strongly sorbed by components in soil (clay, hydrous oxides, organic matter. etc.). These radionuclides are, therefore, relatively immobile in soil and in sediments in natural waters. Most of the plutonium from nuclear weapons testing is concentrated in the upper 5 cm layer of soil and is very likely present in the form of the dioxide. Plutonium, as the PuO2‡ 2 (plutonyl) ion, like calcium, strontium, and radium, is a bone-seeking element. Plutonium-239 resembles 226 Ra by being an a emitter with long biological and radioactive half-lives and is considered to be one of the most radiotoxic radionuclides associated with nuclear power and nuclear weapons. Once in the bloodstream, plutonium tends to concentrate mainly and about equally in the liver and in bone. In addition to isotope dilution, nature provides another way of reducing the human uptake of certain radionuclides. Biological systems have an ability to

655

14. THE NUCLEAR ENVIRONMENT

discriminate against certain elements. The ratio of the 90 Sr concentration in milk to that in forage provides an illustration. Because of the chemical similarity between Sr and Ca, the concentration of 90 Sr in any material can be expressed in terms of a relative unit, the ``strontium unit'' (SU). One strontium unit is equal to 37 mBq (1 pCi) of 90 Sr per gram of calcium. The observed ratio (OR) for 90 Sr in milk relative to that in forage is given by the equation OR ˆ

…90 Sr=Ca† in milk … 90 Sr=Ca† in forage

…14-14†

Under steady-state conditions, the OR values are typically in the range of 0.1±0.2. The SU can be used to follow the dependence of the uptake of 90 Sr in human bone on diet. Biological systems may also concentrate certain elements. Examples of such systems are plants growing in soil and organisms growing in a marine or a freshwater environment. A concentration factor (CF) for aquatic organisms, for example, is de®ned as CO =CW , where CO is the concentration of the nuclear species of interest in the organism and CW is the concentration of the same species in the ambient water. Equilibrium conditions are assumed. For the element zinc, as an example, CF values for plants, mollusks, crustacea, and ®sh in freshwater may be between 10 and 15,000. For similar marine organisms, the CF values for zinc may be between 100 and 300,000. Thus, for a given organism and a given element, the values vary widely with the local conditions.

14.14 DOSE OF IONIZING RADIATION RECEIVED BY THE U.S. POPULATION 14.14.1 Dose from External Exposure External exposure is mainly from x rays (medical and dental), terrestrial g rays (from soil and rocks), and cosmic rays. Most of the a and b particles emitted within a solid or liquid radioactive source are absorbed within the source or in the air, if they escape into the air. Similarly, for a and b radiation emitted by radionuclides in the atmosphere, only the fraction that is emitted close to a person will reach the area of that person's skin not covered with clothing.

14.14.2 Dose from Internal Exposure 14.14.2.1 Natural Radioactivity in Human Body Tissue

The ``reference man'' weighs 70 kg and contains 140 g of potassium …167  10 2 g 40 K† and between 10 10 and 10 11 g of radium. The latter is

656

14.14 DOSE OF IONIZING RADIATION RECEIVED BY THE U.S. POPULATION

in the skeleton and may provide a dose of about 01 mSv=y (10 mrem=y). In soft tissue a dose of about 020 mSv=y (20 mrem=y) comes from the b g radiation of 40 K …127  109 y† and about 038 mSv=y (38 mrem=y) from the a radiation of 210 Po (138.38 d, in uranium series). The contribution from 14 C to the internal dose rate is negligible. 14.14.2.2 Radon

Estimation of the hazard of ``normal'' indoor domestic radon exposure is far more dif®cult than it is for underground miners. Except in rare instances, the level of domestic exposure is much lower and more uncertain; the number of hours of exposure per week is more variable; and the breathing rate is different. Furthermore, the incidence of lung cancer from radon progeny for miners or nonminers who are smokers is superimposed on the incidence of lung cancer attributed to cigarette smoking. Studies of the incidence of lung cancer strongly suggest that there is a synergistic interaction between radon exposure and cigarette smoking. That is, the number of cancers by radon in smokers is greater than that expected from the sum of the effects of smoking alone and radon alone. ``The risk of lung cancer caused by smoking is much higher than the risk of lung cancer caused by indoor radon. Most of the radon-related deaths among smokers would not have occurred if the victims had not smoked.''68 Factors that must be taken into account in the calculation of absorbed dose or dose equivalent include the size of the particles in the inhaled air and the fraction of the radon progeny attached to the particles, the breathing pattern of the individual, and the characteristics of the epithelial cells of the respiratory tract, which are the target cells for lung cancer. Uncertainty in the estimation of the incidence of lung cancer that can be attributed to low-level dose of ionizing radiation from short-lived progeny of radon arises not only from uncertainty in the dose but also from the customary need to extrapolate dose±response curves for stochastic effects from higher level dose data (for underground miners, in this case). The recommended dose limit for radon in the home is based on linear extrapolation and is, therefore, subject to controversy. Doubling the exposure to radon doubles the risk of lung cancer and the Committee on Health Risks of Exposure to Radon, cited in footnote 68, states that ``any exposure, even very low, to radon might pose some risk.'' Furthermore, mathematical models that have been developed to facilitate estimation of the risk of lung cancer from radon exposure necessarily use assumptions that also are controversial. The committee's best estimate, also found in the source cited in footnote 68, ``is that among 68

Committee on Health Risks of Exposure to Radon, Health Effects of Exposure to Radon, BEIR VI, National Academy Press, Washington, DC, 1999.

657

14. THE NUCLEAR ENVIRONMENT

11,000 lung-cancer deaths each year in never-smokers, 2,100 or 2,900, depending on the model used, are radon-related lung cancers. . . . the 15,400 or 21,800 deaths attributed to radon in combination with cigarette-smoking and radon alone in never-smokers constitute an important public-health problem.'' Radon's progeny in air are considered to be the second most important cause of lung cancer, and thus nonsmokers are not ``safe.'' Radon and its progeny also contribute a small fraction of the total number of stomach cancers, as shown earlier in Figure 14-7.

14.14.3 Average Annual Dose Table 14-12 contains a summary of values for the average annual effective dose equivalent +E (Section 13.10.2) of ionizing radiation to a member of the U.S. population. Population density was taken into account in calculating the averages. Note that 82% of the annual dose is from natural sources. It is important to understand that an individual can receive a higher annual effective dose equivalent than the average for the population given in the table. Consider a few examples:

TABLE 14-12 Average Annual Effective Dose Equivalent of Ionizing Radiation Received by a Member of the U.S. Population Source of ionizing radiation Cosmic rays Radon Terrestrial radioactivity (40 K, U series, Th series) Internal (mostly 40 K) X-ray machines (medical diagnostic) Nuclear medicine Consumer products Sleeping partner Otherb Total a

Effective dose equivalent 0.27 mSv (27 mrem) 2.00 mSv (200 mrem) 0.28 mSv (28 mrem) 0.39 mSv (39 mrem) 0.39 mSv (39 mrem) 0.14 mSv (14 mrem) 0.10 mSv (10 mrem) 1 mSv (0.1 mrem)a < 0:01 mSv ( 40 Ci/km2 5 mR/h on May 10 1986

Gden

Pripyat

Vilcha

Nuclear plant

Polesskoye 5

Chernobyl 5

Bober

30 km total exclusion zone

Kiev Reservoir

FIGURE 14-25 Areas of heavy 137 Cs contamination around the Chernobyl exclusion zone (circle) as measured during 1988. The contour marked by isolines indicates the territory where the exposure rate for g radiation was above 5 mR=h on May 10, 1986. From Z. A. Medvedev, The Legacy of Chernobyl, ``map p. 87.'' Copyright # 1990 by Zhores Medvedev. Used by permission of W.W. Norton & Company, Inc.

after the explosions. The zone contained Pripyat, many villages and small settlements, and Chernobyl, a town of about 10,000 inhabitants, located about 18 km southeast of the plant.
About a month after the accident, some soil samples taken in the exclusion zone were found to have 189 TBq=km2 (510 Ci=km2 of 131 I and 100 TBq=km2 (270 Ci=km2 ) of 137 Cs. Plutonium contamination was as high as 037 TBq=km2 (10 Ci=km2 ) near the reactor but did not extend very far except for a few hot spots. The total (worldwide) deposition of 137 Cs was estimated to be about 100 PBq (2.7 MCi).88
About 0.25 million square kilometers of land in an area lying in Belarus, Russia, and Ukraine remained contaminated with 137 Cs at a level of about 37 GBq=km2 (1 Ci=km2 ) some 10 years after the accident.
Two of the workers in the Chernobyl nuclear power plant at the time of the accident on April 26, 1986, died at onceÐone from steam burns and one from falling debris. Two other workers who were sent into the reactor 88

L. R. Anspaugh, R. J. Catlin, and M. Goldman, Science, 242, 1513 (1988).

672

14.16 EXAMPLES OF ACCIDENTS AND INCIDENTS INVOLVING THE RELEASE OF RADIONUCLIDES

building to investigate the accident died of radiation exposure soon after the accident, as did several of the ®remen who received total-body exposure rates over 0258 C kg 1 h 1 (1000 R=h) as they tried to extinguish the burning graphite. Between 197 and 300 of the people who were on the scene at the time of the explosions or soon thereafter as emergency personnel were hospitalized. They received extensive thermal burns and high doses of radiation from external exposure [e.g., up to 16 Sv (1600 rems)] and internal exposure [e.g., 4 Sv (400 rems)] from inhalation of radioactive dust and smoke. Many became incapacitated within a few hours. At least 10 of the patients were given bone marrow transplants; others received liver tissue transplants.  In the town of Pripyat, the exposure rate on the streets was reported to have reached a level as high as about 258  10 4 C kg 1 h 1 (1 R=h).  By July 19, 1986, within days or weeks of the accident, 28 of 35 people who received between 4 Gy (400 rads) and 16 Gy (1.6 krads) had died. In October 1993 the reported death total was 31.  Over 600,000±800,000 people were exposed suf®ciently, either externally or internally, to be registered in a study program set up to follow their health until they die. About 200,000 of these were ``liquidators'' (workers who participated in the cleanup after the accident). The liquidators handled radioactive debris (including graphite from the reactor core) on the plant site or were involved in the construction of the sarcophagus in 1986±1987. Some worked for only 90 seconds. The average dose was reported to be 0.25 Sv (25 rems) during the ®rst year.  Until the residents of Pripyat and about 90,000 other residents of the zone were evacuated from the exclusion zone, they carried out normal outdoor activities (cultivating gardens, etc.), unaware or unafraid of the fallout. Estimates of external doses for individuals living in Pripyat are as high as 0.50 Gy (50 rads) from g radiation and 0.20 Gy (20 rads) from b radiation plus internal doses up to 0.25 Gy (25 rads) to the thyroid.  In Ukraine, 137 Cs contaminated about 6.5 million hectares (about 25,000 mi2 ) of forests and farmland.  Potassium iodide as tablets or as an iodide solution was distributed in Pripyat and nearby areas, in eastern Poland, and in Yugoslavia to decrease radioiodine uptake.89  Because the variable winds at Chernobyl carried the ®ssion products, especially 131 I and 137 Cs, across both eastern and western Europe, some of the milk from dairies in Austria, Hungary, Poland, and Sweden was contaminated (Figure 14-26). Fresh fruit and vegetables, fresh meat, freshwater ®sh, milk, and milk products from countries in eastern Europe90 within 89

There is some evidence that high doses of KI may be harmful. Bulgaria, Czechoslovakia, Hungary, Poland, Romania, the Soviet Union, and Yugoslavia.

90

673

14. THE NUCLEAR ENVIRONMENT

Saturday 26 April 1986

Monday 28 April 1986

Wednesday 30 April 1986

Friday 2 May 1986

Saturday 3 May 1986

Monday 5 May 1986

FIGURE 14-26 Areas covered by the main body of the cloud of radioactive material on various days during the release from the Chernobyl accident. From The Radiological Impact of the Chernobyl Accident in OECD Countries, Nuclear Energy Agency (NEA), Organization for Economic Co-operation and Development, Paris, 1987.

674

14.16 EXAMPLES OF ACCIDENTS AND INCIDENTS INVOLVING THE RELEASE OF RADIONUCLIDES

1000 km of Chernobyl were banned for several weeks by the 12-nation European Economic Community.91 Vegetables grown in parts of France, Greece, and Italy that spring could not be consumed locally or exported as would normally have occurred. Later it was found that in the northern parts of Finland, Norway, and Sweden, where the Lapps raise reindeer for their livelihood, samples of the reindeer meat contained over 80 kBq=kg (216nCi=kg) of radiocesium [134 Cs (2.065 y) and 137 Cs (30.07 y) ]. Maximum values for 137 Cs were about 150,000 Bq=kg for reindeer meat and about 40,000 Bq=kg for lamb. In Norway, bentonite was supplied to farmers as a Cs binder that could be added to animal feed to lower the 137 Cs content of meat and milk. Prussian blue incorporated in salt licks was also used in mountain areas where reindeer, sheep, and goats grazed. Both methods were effective (i.e., a 50±90% reduction in radiocesium contamination was achieved).
In areas of northwest England, north Wales, Northern Ireland, and Scotland, where it was raining when the cloud of radioactivity arrived about a week after the accident, the increase in dose level was about the same as normal background. A few weeks later the cumulative level of 131 I, 103 Ru (39.27 d), 134 Cs, and 137 Cs in sheep exceeded the maximum permissible level of 10 kBq=kg (27 nCi=kg), and the animals were banned as a source of lamb and mutton. Sheep from over 500 farms were still banned some 18 months after the accident.
Dose levels in the then Federal Republic of Germany were probably the highest in western Europe. Again, there were hot spots from rainout in the southern part of the country. Iodine-131 and 137 Cs contamination forced the destruction of leafy vegetables in the areas of highest contamination.
In northern Italy the level of contamination from the same two radionuclides required restrictions on the consumption of milk and vegetables. In France there was normal fallout, requiring restrictions on the use of food until the 131 I level decreased by decay. Fallout was also detected on crops in Greece and Turkey.
Eventually, radionuclides from the accident were detected in the atmosphere over Canada, Japan, and the United States. Evidence for their arrival in Troy, NY is given in Figure 14-27. The spectra show the g-ray activity of particulates in air samples taken over 24-hour periods by standard air-sampling methods in which the particulates were captured on ®berglass ®lters on a rooftop at Rensselaer Polytechnic Institute. The spectra were obtained with a sodium iodide scintillation detector and a g-ray spectrometer set to divide gray energies up to 2 Mev into 200 channels (10 keV=channel).

91 After the ban was lifted at the end of May, imports were still monitored during most of 1987. Intervention limits for 137 Cs were set at 600 Bq=kg for foodstuffs in general and 370 Bq=liter for milk and baby foods.

675

14. THE NUCLEAR ENVIRONMENT

4000

Counts per hour per 10 keV channel

Background

3500 Low-energy scattered photons and high-energy characteristic x rays from (1) members of the Ac, Th, and U series, (2) cosmic radiation, and (3) cosmogenic radionuclides.

3000 2500 2000 1500 1000

K-40 (1.27E+9 y)

500 0 0

50

150

100

200

Channel no.

(a)

Counts per hour per 10 keV channel

4000 3500 Air sample no. 4 05/11/86

3000 2500 2000 1500 1000 500 0 0

50

100

150

200

Channel no.

(b)

FIGURE 14-27 Gamma-ray spectra showing the arrival in Troy, NY, and subsequent decay of ®ssion products from the Chernobyl accident on April 26, 1986. Dates given are when the spectrum was measured. Data provided by H. M. Clark.

14.16 EXAMPLES OF ACCIDENTS AND INCIDENTS INVOLVING THE RELEASE OF RADIONUCLIDES

Counts per hour per 10 keV channel

4000 Air sample no. 5 05/12/86

3500 3000

I-131 (8.0207 d)

2500 2000

Cs-137 (30.07 y) + Ba-137m (2.552 m)

1500 1000 500 0 0

50

100

150

200

Channel no.

(c)

4000

Counts per hour per 10 keV channel

676

3500 Air sample no. 5 05/19/86

3000 2500 2000 1500 1000 500 0 0

50

150

100

200

Channel no. (d) FIGURE 14-27 (Continued)


Spectrum (a) is the background spectrum for the detector, while (b) is that of an air sample taken May 7±8, 1986, before arrival of ®ssion products from Chernobyl. The spectrum (c), for a sample collected May 9±10, shows peaks

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14. THE NUCLEAR ENVIRONMENT

Counts per hour per 10 keV channel

4000 3500 Air sample no. 5 07/05/91

3000 2500 2000 1500 1000 500 0 0

50

150

100

200

Channel no. (e) FIGURE 14-27 (Continuted)

for 131 I (8.020 d) and 137 Cs (30.07 y). When the same sample was counted 7 days later, spectrum (d) was obtained. Spectrum (e) for the same sample a little over 5 years later shows the continuing presence of 137 Cs in secular equilibrium with its daughter 137m Ba (2.552 m). Fission product activity in air samples became undetectable by May 21.
By the end of 1995, the number of cases of thyroid cancer among children in Ukraine that were reported after the accident was about 600 rather than an estimated 50 based on the preaccident rate.
Thyroid doses for 57% of the children who were under one year of age and were living in the exclusion zone were over 2 Gy.
In the heavily contaminated Gomel region of Belarus, an increase in thyroid cancer (presumably from 131 I)92 was observed 4 years after the accident instead of the expected 8±10 years. In 1991 the rate was almost 20 times that of 2 years earlier, and by 1996 the rate was about 200 times the normal rate. The increase in incidence of thyroid cancer in children up to age 15 is the long-term health effect that is accepted as being linked to the Chernobyl

92 Although it is generally believed that 131 I causes thyroid cancer, proof may be found in studies of children in the Chernobyl area. Other shorter-lived iodine isotopes, 132m I (1.39 h), 132 I (2.28 h), 133 I (20.8 h), and 135 I (6.57 h) that were released in the Chernobyl accident are also suspect.

678

14.16 EXAMPLES OF ACCIDENTS AND INCIDENTS INVOLVING THE RELEASE OF RADIONUCLIDES

accident and is beyond the increase that might be expected from intensi®ed levels of examination.93
UNSCEAR 200094 reports that there have been about 1800 cases of thyroid cancer in children who were exposed to ®ssion products (radioisotopes of iodine) at the time of the accident. Additional cases are expected during the next decades.
Initially, the important source of ionizing radiation to the population was 131 I via inhalation or contaminated milk. Later, the hazard shifted to 137 Cs.
A pine forest (500±600 hectares) in the exclusion zone died, as did some of the plants and wildlife.95 Plants and wildlife showed little permanent radiation damage and recovered within about 3 years.
The number of cases of leukemia found up to 10 years after the accident seemed to be less than expected (based on data for Japanese bomb survivors)96 for the exposed population as a whole. UNSCEAR reported that the expected elevation in cases of leukemia was not found 14 years after the accident.
Monitoring of 131 I and 137 Cs provided data indicating that existing models for the movement of these two ®ssion products from the atmosphere into the food chain and for ground migration need to be improved.
The worldwide annual average effective dose from the Chernobyl accident 14 years afterward is estimated to be 0.002 mSv.94
The health and environmental effects of the Chernobyl accident are being studied by a number of international organizations. An International Chernobyl Center (ICC) has been established at the site itself and in the exclusion zone to study radioecology, nuclear safety, and radioactive waste handling. Epidemiological studies are expected to add to our understanding of several health effects, including dose±response relationships associated with ionizing radiation (e.g., thyroid cancer and leukemia). However, uncertainty in dose will be a limiting factor, but less so than for the Japanese survivors.

14.16.3 Radioactive Waste An accident that released signi®cant amounts of radioactive material into the environment occurred in September 1957 at the Chelyabinsk-65 facilities 93 The increase in thyroid cancer was observed sooner than expected (latency of about 10 years). Some critics believe the observed number of cases is too high and is the result of more intensive screening since the accident. 94 United Nations Scienti®c Committee on the Effects of Atomic Radiation (UNSCEAR), UNSCEAR 2000 Report to the General Assembly, United Nations, NY, 2000. 95 Conifers are particularly sensitive to ionizing radiation. These trees received 80±100 Gy. The forest remains contaminated with 90 Sr and 137 Cs. Trees receiving up to about 10 Gy recovered. 96 See reports of the Radiation Effects Research Foundation (RERF), which monitors the health of some 120,000 people who are survivors of the Hiroshima and Nagasaki bombings.

14. THE NUCLEAR ENVIRONMENT

679

located near Kyshtym in the southern Urals in what was then the Soviet Union. The event is variously known as the Urals accident, the Kyshtym disaster, and the Chelyabinsk tragedy. Details of the accident did not become available until 1989. The Chelyabinsk-65 site contained storage and reprocessing facilities for spent reactor fuel, fuel fabrication plants, and facilities for storage and treatment of radioactive waste as part of a complex initially dedicated to the Soviet weapons program. Liquid waste containing ®ssion products as a mixture of nitrates and acetates was stored in several large tanks, which were continuously cooled to remove the ®ssion product heat. Because of problems with the cooling system of one tank, the waste was allowed to evaporate to dryness. The 137 Cs but not the 90 Sr had been removed from the waste. Eventually the temperature of the solid reached about 5008C and the mixture exploded with a force estimated to be that from up to 100 tons of TNT. Most of the approximately 740 PBq (20 MCi) of radioactivity ejected from the tank fell to earth near the site of the explosion. About 74 PBq (2 MCi) moved away from the site as a cloud and contaminated over 200 towns and villages having a total population of about 0.3 million people. In the contaminated areas the 90 Sr activity varied from 37 GBq=km2 to 185 TBq=km2 (01±500 Ci=km2 ). Over 10,000 people were evacuated from the more highly contaminated regions during a period beginning a week after the accident and continuing for several months. Prior to evacuation, many of the people cultivated their gardens as usual and ate the crops. Estimated doses received were up to 1 Gy (100 rads) for individuals at the accident site and up to 3 Gy (300 rads) for people who accumulated their dose in the most contaminated villages during the ®rst month after the accident. The average dose of about 10,000 evacuees was about 50 rems.

14.16.4 Nuclear Fuel Processing Plant On September 30, 1999, a criticality accident occurred in a nuclear fuel processing plant in Tokaimura, Japan. Workers in facilities where ®ssionable materials are handled are given special training to prevent the materials from achieving critical mass. In the Tokaimura accident, the workers used short-cut procedures instead of the licensed, safe procedures in preparing and handling a uranyl nitrate solution containing enriched (18.8%) uranium. Although the uranium oxide was dissolved in buckets instead of the proper vessel, the critical mass needed for the chain reaction was not reached until the workers had transferred 15.8 kg of uranium (seven times the normal amount of uranium) into a tank that had a relatively large diameter and a jacket to allow circulation of cooling water. The water in the solution served as a neutron moderator and that in the jacket

680

ADDITIONAL READING

served as a neutron re¯ector, which scattered neutrons that would have escaped from the container back into the solution and reduced the critical mass requirement. The solution became a nuclear reactor. Normally, the heat generated by the ®ssioning uranium would have caused the volume of the solution to increase, reducing the effectiveness of water as a moderator and reducing the ®ssion rate. Unfortunately, but predictably, the cooling system enabled the reaction to continue for about 17 hours until the cooling water was drained and boron was added to the solution as boric acid. At the moment when the chain reaction began, the solution became an intense source of neutrons and g rays. Volatile ®ssion product radioisotopes of iodine, krypton, and xenon escaped into the room and the ventilating system. Some of the stable 15 N in the air would have been converted to 16 N (7.13 s) by neutron capture. There were three workers in the room at the time of the accident. One who received an estimated dose equivalent of about 17 Sv died 82 days later. The second, who received an estimated dose equivalent of about 10 Sv, died 207 days later. The third received an estimated dose equivalent of 1± 5 Sv and was discharged from the hospital after about 90 days. Other workers (about 148) in the plant received dose equivalents from 1 to 50 mSv. Some 300,000 residents in the area near the plant were warned to stay indoors overnight. This was by no means the ®rst criticality accident. Several resulting in fatalities to workers occurred in the United States during a period of about 20 years beginning with the Manhattan Project in the 1940s. A criticality accident in 1970 at the Kurchatov Institute of Atomic Energy in Moscow resulted in the death of two technicians and very high-level exposure to two others at an experimental critical assembly.

Additional Reading and Sources of Information General Choppin, G. R., J.-O. Liljenzin, and J. Rydberg, Radiochemistry and Nuclear Chemistry (2nd edition of Nuclear and Radiochemistry) Butterworth-Heinemann, London, 1995. Eisenbud, M., and T. Gesell, Environmental Radioactivity from Natural, Industrial, and Military Sources, 4th ed. Academic Press, San Diego, CA, 1997. Various authors, Reports of the (1) Committee on the Biological Effects of Ionizing Radiation, National Research Council, National Academy of Sciences (BEIR reports), (2) Energy Information Administration (EIA), U.S. Department of Energy, (4) International Atomic Energy Agency (IAEA), (4) International Commission on Radiological Protection (ICRP), (5) National Academy of Science-National Research Council (NAS-NRC), (6) National Council on Radiation Protection and Measurements (NCRP), (7) Organization for Economic Cooperation and Development (OECD), (8) Radiation Effects Research Foundation (RERF), (9) United Nations Scienti®c Committee on the Effects of Atomic Radiation (UNSCEAR), (10) U.S. Department of

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681

Energy (DOE), (11) U.S. Environmental Protection Agency (EPA) and (12) U.S. Nuclear Regulatory Commission (NRC). Code of Federal Regulations pertaining to this chapter: Title 10 (Energy), Title 21 (Food and Drugs), Title 29 [Labor (OSHA)], Title 40 (Protection of the Environment), and Title 49 (Transportation). Internet websites. Information on topics covered in this chapter is available from websites such as the following: www.nap.edu (National Academy of Science Press), www.doe.gov (U.S. Department of Energy), www.nrc.gov (U.S. Regulatory Commission), www.epa.gov (U.S. Environmental Protection Agency), www.gpo.gov (U.S. Government Printing Of®ce), and www.nsrb.org (National Radon Safety Review Board).

Radon A Citizen's Guide to Radon, 3rd ed. U.S. Environmental Protection Agency, Document 402-K-92001 (9=92), U.S. EPA, National Center for Environmental Publications (NSCEP), P.O. Box 42419, Cincinnati, OH. (One of many documents available.) Commission on Life Sciences, Committee on Risk Assessment of Exposure to Radon in Drinking Water, Risk Assessment of Radon in Drinking Water, National Research Council, National Academy Press, Washington, DC, 1999. Cothern, R. C., and P. A. Rebers, eds., Radon, Radium and Uranium in Drinking Water, Lewis Publishers, Chelsea, MI, 1990.

Applications of Isotopes Attendorn, H.-G., and R. N. C. Bowen, Radioactive and Stable Isotope Geology, Chapman & Hall, London, 1997. Beck, J. W., et al., Extremely Large Variations of Atmospheric 14 C Concentration During the Last Glacial Period, Science, 292, 2453 (2001). Dickin, A. P., Radiogenic Isotope Geology, Cambridge Univ. Press, Cambridge, U.K., 1995. Geyh, M. A., and H. Schleicher, Absolute Age Determination, Springer-Verlag, Berlin, 1990. Taylor, R. E., Fifty Years of Radiation Dating, Am. Sci.,

(1), 60 (2000). Journals that publish research on isotope fractionation and isotope dating include Applied Geochemistry, Chemical Geology, Earth and Planetary Letters, Environmental Science and Technology, Geochimica et Cosmochimica Acta, Geology, Journal of Climate, Journal of Geophysical Research, Journal of Paleoliminology, Nature, Paleoceanography, Paleogeography Paleoclimatology and Paleoecology, Phytochemistry, Pure and Applied Geophysics, Radiocarbon, Science.

Nuclear Medicine Wagner, H. N., Jr., Z. Szabo, and J. W. Buchanan, eds., Principles of Nuclear Medicine, 2nd ed., W. B. Saunders, Philadelphia, 1995. Journal of Nuclear Medicine (Society of Nuclear Medicine)

Nuclear Reactors and Nuclear Power Plants Bodansky, D., Nuclear Energy: Principles and Practices, American Institute of Physics Press, New York, 1996.

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ADDITIONAL READING

Cochran R. G., and N. Tsoulfanidis, The Nuclear Fuel Cycle: Analysis and Management, 2nd ed., American Nuclear Society, La Grange Park, IL, 1999. Cowan, G. A., A Natural Fission Reactor, Sci. Am., 235, 36, (1976). Glasstone, S., and W. H. Jordan, Nuclear Power and Its Environmental Effects, American Nuclear Society, La Grange Park, Il, 1980. Glasstone, S., and A. Sesonske, Nuclear Reactor Engineering, Vols. 1 and 2, 4th ed., Chapman & Hall, New York, 1994. Murray, R. L., Nuclear Energy: An Introduction to the Concepts, Systems, and Applications of Nuclear Processes, 5th ed. Butterworth-Heinemann, Boston, MA, 2001. Quinn, E. L., New Nuclear GenerationÐIn Our Lifetime, Nuclear News, 44, 52±59 (October 2001). The New Reactors, Nuclear News, 35, 66±90 (September 1992). Report to Congress on Small Modular Nuclear Reactors, Of®ce of Nuclear Energy, Science and Technology, U. S. Department of Energy, Washington, DC, May 2001. U. S. Nuclear Regulatory Commission, Reactor Safety Study, An Assessment of Accident Risks in the U. S. Commercial Nuclear Power Plants, WASH-1400 (NUREG 75=014), 1975.

Cold Fusion Close, F., Too Hot to Handle: The Race for Cold Fusion, Princeton Univ. Press, Princeton, New Jersey, 1991. Taubes, G., Bad Science: The Short Life and Weird Times of Cold Fusion, Random House, New York, 1993.

Nuclear Weapons and Depleted Uranium Carter, L. J., and T. H. Pigford, ``Confronting the Paradox in Plutonium Policies'', Issues XVI (2), 29, (Winter 1999±2000). Also letters to the editor on this paper Issues XVI (3) (Spring 2000), XVI (4) (Summer 2000). Depleted Uranium in Kosovo: Post-Con¯ict Environmental Assessment, United Nations Environmental Programme (UNEP), United Nations, New York, 2001. Jeanloz, R., Science-Based Stockpile Stewardship, Phys. Today, 53, 44 (2000). Of®ce of Technical Assessment, Congress of the United States, Nuclear Proliferation and Safeguards, Praeger, New York, 1977. Sullivan, J. D., The Comprehensive Test Ban Treaty, Phys. Today, 51, 24±29 (1998).

Radioactive Waste Committee on Separations Technology and Transmutation Systems, Nuclear Wastes: Technologies for Separations and Transmutation, National Academy Press, Washington, DC, 1996. Macfarlane, A., Interim Storage of Spent Fuel in the United States, Annu. Rev. Energy Environ., 26, 201±235 (2001). Murray, R. L., Understanding Radioactive Waste, 4th ed., Battelle Press, Columbus, OH, 1994. Radioactive Waste, Phys. Today, 50, 22±62 (1997). Wiltshire, S. D., The Nuclear Waste Primer, rev. ed., League of Women Voters Educational Fund, Washington, DC, 1993.

Sources and Effects of Ionizing Radiation Committee on the Biological Effects of Ionizing Radiation (BEIR), The Health Risks of Radon and Other Internally Deposited Alpha-Emitters, BEIR IV, 1998; Comparative Dosimetry of Radon

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683

in Mines and Homes (companion to BEIR IV), 1991; Health Effects of Exposure to Low Levels of Ionizing Radiation, BEIR V, 1990; Health Effects of Exposure to Radon, BEIR VI, 1999, National Research Council, National Academy Press, Washington, DC. Hendee, W. R., and F. M. Edwards, eds., Health Effects of Exposure to Low-Level Ionizing Radiation, Institute of Physics, London, 1996. Moeller, D. W., Environmental Health, Harvard University Press, Cambridge, MA, 1992. Peterson, L. E., and S. Abrahamson, eds., Effects of Ionizing Radiation: Atomic Bomb Survivors and Their Children (1945±1995), Joseph Henry Press, Washington, DC, 1998. UNSCEAR (United Nations Scienti®c Committee on the Effects of Atomic Radiation), Reports to the General Assembly of the United Nations, United Nations, NY: UNSCEAR 1988 (includes Chernobyl) UNSCEAR 1993 UNSCEAR 2000 Vol. I: Sources, Vol. II: Effects (Both volumes include Chernobyl update)

Chernobyl Kryshev, I. I., ed., Radioecological Consequences of the Chernobyl Accident, Nuclear Society International, Moscow, 1992. Medvedev, Z., The Legacy of Chernobyl, Norton, New York, 1992. Mould, R. F., Chernobyl Record, Institute of Physics, London, 2000. (Contains updated data on levels of radioactivity and effects on the population.) Vargo, G. J., ed., The Chernobyl Accident: A Comprehensive Risk Assessment, Battell Press, Columbus, OH, 2000. (Contains details about the accident and its effects written by a group of Ukrainian scientists.)

EXERCISES 14.1. What is the heat output (watts) associated with the a decay of a sample containing 1 kg of (a) 235 U (t1=2 ˆ 704  108 y), Ea ˆ 44 MeV; (b) 239 Pu (t1=2 ˆ 2410  104 y), Ea (ave) ˆ 5.13 MeV; (c) 238 Pu (t1=2 ˆ 877 y), Ea ˆ 55 MeV? Ç (Gy/h) in 100 g of soft tissue containing 21  106 Bq of 14.2. Calculate D 14 3 (a) C, (b) H. [See Equation (13.68).] 14.3. Show that the theoretical separation factor for enriching 235 U in natural uranium by gaseous diffusion is 1.0043. 14.4. How many kilograms of D2 O would be required per year to replace the D2 O consumed by the (d,d) reaction in a thermonuclear power plant with an output of 4000 MWt? 14.5. How many grams of 3 H would be ``burned'' if the D-T reaction is the source of energy for the power plant in Exercise 14.4? 14.6. Show that the power density of a sample of 90 Sr that is a month old is 0.93 W=g. (See Figure 13.13.) 14.7. Look up the composition of granites, choose one and calculate the heat output in watts from the 40 K for a metric ton of the granite. The

684

EXERCISES

14.8.

14.9.

14.10.

14.11.

14.12.

14.13.

14.14.

14.15. 14.16.

14.17.

14.18.

abundance of 40 K is 0.0117 at. % and the decay scheme is given in Figure 13-15. Look up and summarize any changes that have been made during the past 12 months in the Code of Federal Regulations (CFR) for DOE, NRC, EPA, and FDA that apply to the topics covered in this chapter. In a poll taken in 1992, it was found that 36% of the U.S. population believed that milk containing radioactive contaminants could be made safe by boiling it. Comment on the validity of the belief. How do you account for so considerable a percentage of the population having such a belief? At a time prior to 1952, when the speci®c activity of 14 C in new wood was 15.3 disintegrations per minute per gram of carbon, how old was a sample of wood having a speci®c activity of 9.7 dpm? If the forest vegetation and soils on the earth contain approximately 114  1018 g of carbon, what is the corresponding 14 C activity in on becquerels and curies? Assume the speci®c activity in given in Exercise 14.10. If the total global inventory of 14 C is about 83  109 GBq and the rate of production in the atmosphere is about 92  105 GBq per year, is the inventory increasing or decreasing? At what rate? If the standard 70-kg man contains 12.6 kg of carbon and the speci®c activity given in Exercise 14.10 is assumed, how many b particles are emitted in his body per year? Boiled cod®sh contains about 200 mg of potassium per 100 g of ®sh. If you eat 200 g of cod®sh, how many becquerels and curies of 40 K will you ingest? (See Exercise 14.7.) Explain how ®ssion products could appear in the steam turbines of a PWR power plant. A sample containing 235 U is irradiated with slow neutrons for one year. After a decay period of 109 seconds, it is found that 99.6% of the decay heat is produced by four ®ssion products, Which are they? Why are 99 Tc and 129 I not among the four? If the fuel in an LWR contains 7.4 PBq (0.20 MCi) of 131 I per metric ton of heavy metal after an irradiation of 200 days, what will the activity of 131 I be if the irradiation is continued for another 50 days? If the fuel that has been irradiated for 200 days is ``cooled'' for 150 days, what will be the 131 I activity? If a mixture of spent fuels stored in a repository contains 100 g each of 90 Sr (28.78 y), 137 Cs (30.07 y), 239 Pu (2410  104 y), and 241 Am (432.7 y), what will be the activity of each in becquerels and curies after 10,000 years?

14. THE NUCLEAR ENVIRONMENT

685

14.19. Assume that over a period of time the total quantity of 99m Tc (6.01 h) given to many patients is 370 PBq (10 MCi). In becquerels and curies, how much 99 Tc (213  105 y) is added to the environment? 14.20. It is found that d18 O values remain fairly constant as measurements are made for samples taken deeper in an ice core until a certain depth is reached, at which point the value begins to drop until it reaches a new average value about 15% lower. What does this reveal about the environment? 14.21. Much has been learned about salt domes from centuries of salt mining. Describe typical salt domes in some detail. What are the desirable and undesirable properties of salt domes as receptacles for storage of radioactive waste? 14.22. What is the ratio of 235 U=238 U today? Calculate what the ratio would have been 2 billion years ago when the all-natural Oklo reactors were operating. What is it for fresh fuel in an LWR? Why was the presence of water important at the Oklo sites? 14.23. Is the weight of ®ssion products in spent LWR fuel greater or less than the weight of 235 U ®ssioned? Explain. 14.24. Prepare an essay, a class presentation, or a term paper on one of the following. (a) The methods currently being funded in the United States, in Europe, and in Asia to develop thermonuclear energy. (b) Current concepts of thermonuclear power reactors in the future. (c) The design features of a nuclear power plant under construction or placed in operation in any country during the past 12 months that qualify it as having an ``advanced'' design. (d) Latest values for concentration factors for plants, animals, ®sh, etc. Comment on the ranges of values for a given species. (e) The latest radiopharmaceuticals available for diagnosis. (f) The latest radiopharmaceuticals available for therapy. (g) Your conviction about food irradiation. Give reasons. (h) The types and locations (worldwide) of nuclear power plants under construction. (i) The status of accelerator disposal of waste from spent fuel from nuclear power reactors. (j) Current thinking about the health hazard posed by 222 Rn. (k) Recent examples of studies using isotope fractionation. (l) Recent examples of age determination that are relevant to the environment. (m) Recent accidents involving high-level sources (e.g., industrial or therapy).

686

EXERCISES

(n) Recent accidents involving nuclear reactors of all types. (o) Recent changes in federal and=or state regulatory limits for dose of ionizing radiation. (p) Recent changes in the half-life values for the radionuclides 3 H, 7 Be, 14 C, 40 K, 90 Sr, 137 Cs, and 239 Pu. 14.25. Prepare an essay, a class presentation, or a term paper on the current status of one of the following. (a) Oklo reactors and mining of uranium in the region (b) WIPP (c) Yucca Mountain repository and geologic repositories in other nations. (d) Health of people exposed to ionizing radiation tracable to the Chernobyl accident (e) Environmental effects of the Chernobyl accident (f) 99m Tc radiopharmaceuticals (g) New uses for radiopharmaceuticals (h) New radiopharmaceuticals other than those of 99 Tc (i) Radiotherapy (j) Use of particle accelerators for radiation therapy (k) Radioactive waste at Hanford or another facility (l) Radioactive waste disposal in Europe and in Asia (m) Food irradiation in the United States (n) Food irradiation in Europe and in Asia (o) Low-level waste disposal (especially for medical facilities) in your home state or country (p) Studies of the survivors of Hiroshima and Nagasaki (q) High-temperature, gas-cooled reactors (r) Use of MOX to reduce the stockpile of weapons-grade plutonium (s) Proliferation of nuclear weapons (t) CTBT: Which nations have signed the treaty? Which nations have rati®ed it? Which nations are eligible, but have not yet signed it? (u) Reduction of stockpiles of nuclear weapons worldwide (v) ``The nuclear deterrent'' (w) Cold fusion (x) Origin and health effects of cosmic radiation (y) Status of breeder reactors (z) Advances in the applications of MRI and fMRI and radiopharmaceuticals for medical diagnosis

15 ENERGY

15.1 INTRODUCTION Human societies have always required energyÐfor cooking and heating, for transportation, and for industrial activities. For most of human existence, wood has provided the main fuel for cooking, heating, and such high-temperature techniques as pottery and metallurgy. Human and animal power have provided the mechanical energy, supplemented from some ancient time by wind and water power as windmills and water wheels were developed. But it was only with the invention of the steam engine and later the internal combustion engine and electrical generators, all with a need for an energy supply, that power for technological development became freely available. Transportation similarly was by muscle or wind power until these other power sources were developed. Use of wood as a major energy source resulted in deforestation and large environmental changes when population density became large; some third-world nations have serious problems today from demands for wood as cooking fuel that outstrip regeneration. For other uses, wood is a relatively inef®cient and variable fuel. Even primitive technologies attempted to improve on it by the use of charcoal: partially burned wood from which the volatile 687

688

15.1 INTRODUCTION

components have been driven off and the solid converted to nearly pure carbon. Industrialization required the use of a superior fuel, coal, which became the main fuel for industrial and mechanized transportation applications. Coal is abundant, but much less convenient than liquid fuels such as petroleum. Widespread availability of the latter permitted it to replace coal in most transportation and some stationary power generation and heating applications by the mid-twentieth century. More recently, natural gas has been playing a larger role. After 1945, nuclear energy from ®ssion began to be considered as a major component of power generation, and in some nations (e.g., France) ®lls that role today, although in other nations public concern about safety and general fear of radiation make its future questionable. Still more recently, attention has shifted to liquid fuels that are readily prepared from biological sources (e.g., alcohols), mainly for environmental reasons. All these sources of energy are ®nite, and in the case of petroleum in particular, reserves are projected to have limited lifetimes at present rates of use, although predictions of when we will exhaust them have repeatedly been shown to be wrong as more reserves have been discovered. The need to conserve these limited resources is one reason to use them with more ef®ciency and to ®nd alternative, preferably renewable sources. Another reason, and one that has driven a great deal of research and development in recent years, has been the realization that availability of much of these resources is controlled by a small number of nations, which consequently wield considerable power to in¯uence world events. This was brought out in the ``oil crisis'' of the early 1970s, when the large Middle East producers cut production to drive up prices. Not only did prices for petroleum products and materials dependent on petroleum for their production go up, but severe shortages developed that resulted in restrictions on driving and, in some places, gasoline being available only on alternate days of the week. Still another reason to look for alternatives to the traditional fossil fuels is concern about environmental degradation that accompanies their use, as we have discussed many times. Human need for energy has had and will have major impacts on the environment. Much of our energy is based on combustion of carbon-based fuels. The energy released upon combustion is essentially the difference between the energy of the bonds that are formed in the product molecules (CˆO and OÐH) and those in the reactants that are broken (OˆO in dioxygen, and CÐC, CÐH, CÐO, etc., depending on the fuel). Some illustrative values of heats of combustion (heating values) are given in Table 15-1 for equal masses of material. Wood and some coals can be highly variable because of moisture content. Note that heating values for oxygenated fuels are lower than for others because some of the bonds that appear in the products (OÐH) are already present in the reactants.

689

15. ENERGY

TABLE 15-1 Heating Value for Various Fuels Fuel Methane Propane n-Butane Gasoline, kerosene Fuel oil Coal anthracite Bituminous Lignite Wood (12% moisture) Methanol Ethanol

Heating value (kJ=g) 55.6 50.3 49.5 41±48 44.4±49.4 32.5 25.5±34.8 11.6±17.4 17.5±18.3 22.7 29.7

In this chapter, we shall discuss some thermodynamic considerations underlying ef®ciency, and then consider the various sources of energy that are in use or that are reasonable proposals for future use. Not all these are chemical, but we shall include them for completeness. We shall also comment on some predictions for future energy needs.

15.2 THERMODYNAMIC CONSIDERATIONS 15.2.1 The First and Second Laws of Thermodynamics Energy ¯ow and energy use are governed by the law of conservation of energy, which states that energy can neither be created nor destroyed, although it can be changed from one form to another. This law appears sometimes as the ®rst law of thermodynamics: DU ˆ q ‡ w

…15-1†

where DU is the change in internal energy of the system being studied when heat q ¯ows in or out, and work w is done on or by the system. The system being studied can be any part of the universeÐa person, a city, a forest, a gasoline engine, a nuclear power plantÐwithin certain limits that will not be discussed further here.1 All the rest of the universe is called the surroundings. When DU is positive, the internal energy of the system is increasing; when it 1

For rigorous application of the laws of thermodynamics, the system in question must have either isothermal or adiabatic boundaries at any time.

690

15.2 THERMODYNAMIC CONSIDERATIONS

is negative, the internal energy of the system is decreasing. When q is positive, heat is being absorbed by the system from the surroundings; when it is negative, heat is being evolved by the system to the surroundings. When w is positive, work is being done on the system by the surroundings; when it is negative, work is being done by the system on the surroundings. There are many forms of work. For example, mechanical work can be done on the system by compressing it, or the system can do mechanical work on the surroundings by expanding against a resisting pressure. Electrical work can be done on a charged particle by moving it through a potential difference. Most of the time we will be concerned here only with the mechanical work of expansion or compression of a system from volume Vi to Vf against a resisting pressure P, in which case Z Vf wˆ PdV …15-2† Vi

If the resisting pressure P is constant, w ˆ PDV, where DV … ˆ Vf Vi † is the change in volume of the system when it expands …DV > 0, w < 0† or is compressed …DV < 0, w > 0†. We shall be discussing the heat released during various chemical reactionsÐfor example, the combustion of coal or oil. The enthalpy H of the system is de®ned as H ˆ U ‡ PV, so that the change in enthalpy for a process is DH ˆ DU ‡ D…PV†. If we consider only the mechanical work of expansion or compression, it is easily shown from equation (15-2) that at constant pressure the heat absorbed for a process is equal to the change in enthalpy: qp ˆ DH

…15-3†

A heat engine is a device that generates mechanical work from heat. An example is the automobile internal combustion engine, in which chemical energy is released as heat at about 1000 K when gasoline is burned in the combustion chamber above the pistons. Some of this heat appears as work as the pistons move and drive the transmission, generator, and so on through a complex series of linkages, and much heat is ``rejected,'' some at the temperature of the exhaust, and some at the temperature of the cooling system. When a car is cruising down a highway at about 50 mph (80 km=h), about 75% of the chemical energy is lost as ``rejected'' heat, and only about 25% of the chemical energy is eventually converted to useful mechanical work to move the automobile. The automobile internal combustion engine operates through a sixprocess cycle called the Otto cycle.2 In the following discussion, however, we 2 M. W. Zemansky and R. H. Dittman, Heat and Thermodynamics: An Intermediate Textbook, 7th ed., McGraw-Hill, New York, 1997.

691

15. ENERGY

q1

Reversible isothermal expansion at T1

q=0

Step IV

Step I

Reversible adiabatic compression

q=0

Reversible adiabatic expansion

Step II

Reversible isothermal compression at T2 q2

Step III

FIGURE 15-1 Schematic diagram of the Carnot cycle.

will use a simpler hypothetical heat engine that operates reversibly3 through a four-step cycle that is known as the Carnot cycle. We have seen that the ®rst law of thermodynamics states that energy can be changed from one form to another but that it cannot be created or destroyed; it says nothing about how much one form can be changed to another. The second law of thermodynamics puts a limit on the amount of heat that can be converted into work. Speci®cally, one statement of the second law is that no process is possible in which the sole effect is the conversion of heat into work.4 A corollary of this is that a heat engine operating through a cyclic process must undergo heat transfers with at least two heat reservoirs at different temperatures. Consider now the Carnot cycle (Figure 15-1). It operates reversibly between two temperatures, a high temperature T1 and a low temperature T2 . (The Otto cycle requires more than two reservoirs.) A quantity of heat q1 is absorbed isothermally at T1 from the high-temperature reservoir by reversibly expanding a gas (step I), and work is done on the surroundings as the gas is cooled by reversible adiabatic (no heat absorbed) expansion from T1 to T2 (step II). To complete the cycle (return to the starting conditions), the gas is 3

A reversible process by a system is carried out in such a manner that at any stage, the direction of the process may be reversed by an in®nitesimal change in the conditions of the surroundings. It is required by the second law that all naturally occurring (spontaneous) processes be irreversible. 4 Of course, many processes are possible in which heat is converted completely into work. An example is the isothermal expansion of an ideal gas from Vi to Vf . There is no change in internal energy, so that all the heat absorbed by the gas is converted to work performed by the gas on the surroundings. However, this is not the sole result of the process (i.e., the gas has also expanded) and therefore the second law of thermodynamics is not violated.

692

15.2 THERMODYNAMIC CONSIDERATIONS

compressed isothermally at T2 , evolving heat q2 to the low-temperature reservoir (step III), and ®nally is adiabatically compressed back to the high temperature T1 with some work being done on the gas (step IV). The ef®ciency of a heat engine Z is de®ned as the net work output (work done on the surroundings) divided by the heat input at the high temperature: wnet …15-4† Zˆ q1 Thus, for the reversible Carnot cycle operating with no frictional or other losses (i.e., operating under maximum ef®ciency conditions), it can be shown5 that Zmax ˆ

T1

T2 T1

…15-5†

where T1 and T2 must be in kelvin. It turns out, in fact, that Zmax is the maximum ef®ciency for any heat engine operating between two temperatures. Thus, the maximum ef®ciency depends on the difference between the two temperatures, T2 T1 , at which the engine operates; it becomes more ef®cient as the temperatures T1 and T2 move farther apart. Since, for most purposes, room temperature (300 K) is usually the lowest practical value for T2, much effort has been expended to make T1 as high as possible for various engines. For example, superheated steam, rather than ordinary steam has been used in steam engines (high pressures are necessary for this). The important thing to note here is that there is a theoretical maximum ef®ciency for engines that do useful work [equation (15-5)]; an actual engine running between these two temperatures generally will have an ef®ciency considerably less than this maximum possible ef®ciency because it operates irreversibly and has various other losses. We have seen, for example, that an engine in an automobile being driven under highway conditions has an ef®ciency of approximately 25%. If this engine could be assumed to be operating as a reversible Carnot cycle engine between 1000 and 300 K, its ef®ciency would be 70%. The secondlaw limitation becomes even more important when the high-temperature heat source is at a much lower temperature, such as geothermal, or nonfocused solar sources, or bodies of water. It is pointed out in Section 15.5.3.3, for example, that solar ponds have at most a temperature gradient of about 508C, giving a maximum second-law ef®ciency of the order of 15%. If a Carnot cycle heat engine is reversed so that a net amount of work is done on the system accompanied by withdrawal of an amount of heat q2 from the low-temperature reservoir, the net effect is the transport of an amount of heat from the low-temperature reservoir to the high-temperature reservoir by the expenditure of work. This is the principle behind the heat pump that is used 5

See any elementary physical chemistry textbook: for example, R. A. Alberty and R. J. Silbey, Physical Chemistry, 3rd ed., Wiley, New York, 2001.

693

15. ENERGY

in many areas for domestic heating of buildings. (It is also the principle of an electric compressor refrigerator.) The outside of the building is the lowtemperature reservoir at T2 and the inside is the high-temperature reservoir at T1 . The minimum amount of work that would have to be done (e.g., electric work to run a compressor) to pump q2 heat from the outside to the warmer inside can also be shown to be wmin ˆ q2

T1

T2 T2

…15-6†

Thus, consider a building being maintained internally at 228C (295 K) with an outside ambient temperature of 58C (268 K). From equation (15-6), only a minimum of about 100 J of electric work would have to be expended in order to pump 1000 J of heat into the building, or about 10% of the energy required if the 1000 J of heat was supplied to the building at maximum ef®ciency by electric resistive heating. It is important to emphasize that the maximum ef®ciency limitation given by equation (15-5) is a second-law limitation restricted to the conversion of heat into work. Other parts of the overall conversion from chemical to electrical energy are generally much more ef®cient than the heat-to-work component. Combustion ef®ciency can be as high as 98%, boiler heat transfer ef®ciencies are typically 80±90%, and mechanical-to-electrical is often greater than 90%. If heat is not involved, the second-law limitation does not apply, although the ®rst law conservation of energy limitation will still be applicable. The direct conversion of solar energy to electrical energy (see Sections 15.5.4 and 15.5.5) and of chemical energy to electrical energy as in fuel cells (Section 15.9) are examples of such processes, as are conversions of wind or wave energy to electrical energy. However, other limitations on the ef®ciencies of some of these processesÐfor example, restrictions on the ef®ciencies of solar photovoltaic cells (Section 15.5.4)Ðmay be even more restrictive than the second law. Indeed, at the present time virtually all the chemical energy of fossil fuels and the nuclear energy of ®ssile fuels is ®rst converted to heat before being converted to mechanical (and then on to electrical) energy. The waste heat from our various engines is usually rejected into the environment and there becomes ``thermal pollution,'' although in some cases this ``rejected'' heat is used as a by-product for domestic or industrial heating. We saw in Chapter 3 that cities are always warmer than their surrounding countryside partly because of the rejected heat from all the machines and engines used in the city. Large electric power plants, whether of the steam or nuclear type, reject their waste heat into a very small volume of the environment. When these power plants are water cooled, the streams and lakes into which this water is usually released may become much warmer and change the environment for aquatic life. Large populations of ®sh may be killed, or, alternatively, attracted by the new, warmer environment.

694

15.3 FOSSIL FUELS

15.2.2 Units of Energy and Power In this book we generally use the SI system of units, in which the unit of energy is the joule (J) and the unit of power (energy per unit time) is the watt (W): 1 W ˆ 1 J=s ˆ 3600 J=h. However, so many other units of energy and power are in common use that some useful conversion factors are given here: 1 J ˆ 10 3 kJ ˆ 10 6 MJ ˆ 10 9 GJ ˆ 10 12 TJ ˆ 10 15 PJ ˆ 10 18 EJ …k ˆ kilo; M ˆ mega; G ˆ giga; T ˆ tera; P ˆ peta; E ˆ exa† 1 J ˆ 107 ergs ˆ 0:239 cal ˆ 9:48  10 4 Btu ˆ 2:778  10 4 Wh 1 cal ˆ 4:184 J 1 Btu ˆ 1054 J ˆ 1:054 kJ 1 W ˆ 44:27 ft-lb=min ˆ 1:341  10 3 HP 1 kWh ˆ 1000 Wh ˆ 3:6  106 J ˆ 3600 kJ 1quad…Q† ˆ 1015 Btu ˆ 1:054  1018 J ˆ 2:93  1011 kWh Since the conversion of thermal energy (heat) to mechanical and ultimately to electrical energy is limited by the second law, thermal energy (designated by subscript ``th'') is often referred to as low-grade energy and electrical energy (subscript ``e'') as high-grade energy. It always takes more than 1 kWhth heat from the combustion of coal or from any other fuel to produce 1 kWhe of electricity from a fuel-®red electric power plant, not only because of the second-law limitation but also because no real process is as ef®cient as a hypothetical reversible cycle.

15.3 FOSSIL FUELS 15.3.1 Introduction Fossil fuels in the form of coal, petroleum, and natural gas account for 90% of all the energy used in the United States (Section 15.10.1). The growth in the use of fossil fuels as an energy source has been very rapid, as evidenced by the fact that wood supplied 90% and coal only 10% of the energy used in the United States in 1850. Coal and wood supplied equal proportions of energy in 1885. Undoubtedly this change from wood to coal re¯ected the greater ease in obtaining large amounts of coal required for the new industries developing in the United States. However, some of the incentive for the change may have also been the ``energy crisis'' resulting from cutting down most of the readily available trees in the eastern United States. Petroleum, coal, and natural gas are expected to continue to be the dominant energy sources in the United States and the rest of the world well into the twenty-®rst century (Figure 15-2). An optimistic estimate of the world's oil

695

15. ENERGY

Annual quads 1500

Solar and new sources

1000

Hydro

Conservation

Nuclear

500

Natural gas Oil Coal 0 1980

2000

2020

2040

2060

FIGURE 15-2 Projected global primary energy production by energy type (conservative case). Coal remains the primary fossil fuel source, with a rise and eventual decline of oil and growing levels of energy from natural gas, uranium, solar, and other (e.g., biomass) sources. From C. Starr, M. F. Searl, and S. Alpert, Energy sources: A relative outlook, Science, 256 981±987. Copyright # 1992 American Association for the Advancement of Science.

reserves was published by the U.S. Geological Survey in 2000 which indicates that there is 20% more oil to be discovered in the world than was estimated in 1994 (Figure 15-3). In this estimate the world's oil production will peak in 2050, while the more pessimistic 1994 estimate is 2015. The pessimists note that global oil consumption is 27 billion barrels a year and is increasing by 1.5± 2% each year. The postulated and undiscovered reserves are estimated to amount to about 2300 million barrels, with the United States having about 8% of that. The projected U.S. reserves were doubled in previous estimates, but the new estimates note no further increases. The extraction of oil from these U.S. reserves will be more costly because more expensive technologies will be required to retrieve the remaining oil. There was little change in the estimates of coal reserves in this time period, and the current supply of coal is suf®cient to meet all our energy needs for the next 200 years. In 1999 coalpowered generators accounted for 56% of the electricity produced in the United States and 36% in the world. Energy conservation is projected to be the biggest ``energy source'' from about 2020 on into the future. That is, projected future energy needs, based on current practice, will be reduced by greater ef®ciency.

696

15.3 FOSSIL FUELS

1500

Billion barrels of oil

1000

Undiscovered conventional Remaining reserves Cumulative production

800 600 400 200 0

Former Soviet Union

Middle East and North Africa

Asia Pacific

Europe

North Central SubSouth America and South Saharan Asia (excl. U.S.) America Africa and Antarctica

FIGURE 15-3 The amounts of oil already produced, known to be in the ground, and yet to be discovered in the world. Estimates for the United States are not included in this ®gure but can be found in earlier estimates. Redrawn from R. A. Kerr, Science, 289, 237 (2000).

15.3.2 Liquid Hydrocarbon Fuels 15.3.2.1 Petroleum

Oil is a convenient energy source because it can be obtained cheaply, it is easy to transport, and, when burned properly, it produces low levels of environmental pollutants. The technology for the separation and conversion of crude oil into a variety of hydrocarbon fractions is well worked out (Section 6.2). Unfortunately the tremendous use of petroleum in the United States has resulted in the consumption of over 50% of our known reserves and, as a consequence, the rate of U.S. crude oil production is decreasing. The country has imported over 50% of its crude oil since 1997 to supplement the diminished domestic supply. 15.3.2.2 Tar Sands and Oil Shales

Products very similar to those obtained from crude oil may be obtained from tar sands and oil shales. The potential for petroleum production from these sources is estimated to be equal to that of all the crude oil reserves in the world. However, in most instances, the cost of the recovery of this petroleum in 1998

697

15. ENERGY

is not competitive with the simple extraction of oil and gas. Oil shales and tar sands may be an important source of petroleum by the middle of the twenty-®rst century, when the cost of crude oil increases because of its diminishing supply. Tar sands are a mixture of approximately 85% sand and 15% hydrocarbons, chie¯y the heavier fractions of crude oil. The hydrocarbons have the consistency of paving asphalt. There are large deposits of this black sand in Alberta, Canada, and in Venezuela, and smaller ones in the western United States. Some of the tar sands can be obtained using open-pit mining techniques. The hydrocarbon±tar mixture is then stirred with NaOH and surfactant to give a frothy foam that contains the hydrocarbons. This foam scraped off the top and the sand are sent to settling ponds. The tar is then cracked and re®ned to give oil (Section 6.2). Suncor Energy of Fort McMurray, Alberta, Canada, produces and pro®tably sells 28 million barrels of oil annually using this procedure.6 However, most of the tar sands deposits are so deep that other methods must be used to extract them. The approach looked on with favor at the present time is to warm the tar by injecting steam into the bed; the hot oil forms pools in the vicinity of the injected steam and can be pumped to the surface and processed like crude oil. The largest oil shale deposits (sedimentary rock containing hydrocarbon material) in the world are located in Utah, Colorado, and Wyoming. The organic portion of shale oil is a highly cross-linked material called kerogen. Consequently, the shale must be heated to crack this hydrocarbon so that the organic products may be removed from the shale. When shale is heated, gaseous hydrocarbons, an oil, and a cokelike residue are obtained. The oil can be processed in the same fashion as natural petroleum (Section 6.2), while the residual coke is used as an energy source to thermally crack the kerogen in more shale rock. 15.3.2.3 Synthetic Petroleum Products from Coal

The conversion of coal to petroleum has been investigated sporadically for over 60 years. Germany obtained some of its petroleum by this means during World War II. South Africa has been preparing petroleum this way since the mid-twentieth century. At present the United States is only testing potential coal liquefaction techniques at the pilot-plant level. This process is discussed in more detail in Section 6.9.3.

15.3.3 Coal About 25% (Figure 15.2) of the energy produced in the United States and in the world is generated from coal. Unfortunately severe environmental problems 6

R. L. George, Mining for oil, Sci. Am. pp. 84±85, March 1998.

698

15.3 FOSSIL FUELS

may result from using greater amounts of coal in energy production. One major problem is the release of oxides of sulfur when coal is burned. Bituminous coal from the eastern and midcontinent United States usually has a high sulfur content (3±6%). About half the sulfur in coal is in the form of pyrite (FeS2 ), of which about 90% can be removed by mechanical cleaning; but the remainder of the sulfur is covalently bound to the carbon and can be removed only by chemical reaction. If this high-sulfur coal is used, then the sulfur oxides (mainly SO2 ) must be removed from the stack gases after the coal is burned, or the coal must be chemically changed (e.g., coal gasi®cation or liquefaction) in such a way that the covalently bound sulfur can be removed. The removal of SO2 from stack gases has been studied for many years, but the technology that has been developed is still controversial (Section 10.4). The method that is generally considered to be the most ef®cient is the use of limestone to absorb the SO2 . The main drawback is that up to 350 lb (159 kg) of limestone is required to absorb the SO2 emissions from a ton of high-sulfur bituminous coal. As a consequence, 8 9 ft3 (0:2 0:3 m3 ) of sludge, which must be disposed of, is produced per ton of coal processed. A second problem associated with coal combustion is the formation of nitrogen oxides. This formation is enhanced by the need to carry out the combustion at near 15008C to get high thermal ef®ciency. A third problem is the release of toxic heavy metals, e.g., Hg, Pb, and Cd present at low levels in coal. There are calls for restrictions on Hg emissions from coal burning plants (Section 10.6.6).

15.3.4 Natural Gas Natural gas is a nearly ideal fuel (Table 15-1). Gas is virtually pollution free; it is easy to transport by pipeline, and it requires little or no processing after it comes from the gas well (although some sources contain H2 S that must be removed). Natural gas consists mainly of methane together with some other low molecular weight hydrocarbons. In 1997 it supplied about 23% of the energy requirements of the United States. In 2000 the worldwide reserves of natural gas were estimated by the U.S. Geological Survey to be about 85% of those of petroleum in energy content, and the United States had about 8% of this total amount. These reserves are postulated to last longer because the rate of their consumption is slower than that of oil. The use of natural gas in place of coal or oil has many environmental bene®ts. It usually contains virtually no sulfur or sulfur compounds, so its combustion does not contribute to the emissions of SO2 and its use contributes only 13% of the U.S. NOx emissions, while coal and oil contribute 84%. Being the least carbon intensive of the fossil fuels, upon combustion it contributes the least amount of carbon dioxide per unit of energy.

699

15. ENERGY

15.3.5 Synthesis of Methane from Coal A commercial-sized plant for the conversion of coal to methane, the Great Plains Gasi®cation Facility in Beulah, North Dakota (Figure 15-4), has been in operation successfully since 1984. It is the outcome of ®ve U.S. pipeline companies' desire to have an alternative supply of methane gas and the U.S. Department of Energy's interest in having a domestic synthetic fuels demonstration facility built. After default on the loan by the original owners, the project reverted to the Department of Energy for three years. It was purchased by the Basin Electric Cooperative in 1988 and is run as both a commercial source of SNG (substitute natural gas, or methane) and as a demonstration facility to investigate the development of various by-products. The SNG is made from lignite coal that is strip-mined nearby, and the facility processes about 32,000 tons of lignite a day. The ®rst step is to crush and screen the coal. The larger pieces (17,000 tons=day) are used for methane formation, while the ®nes (up to 15,000 tons=day) are sent to a nearby power plant for the generation of electricity. The coal is gasi®ed in 14 Lurgi reactors [Section 6.9.2, equations (6-9)±(6-11) ] in the presence of oxygen and steam. The oxygen is separated from other atmospheric constituents in a cryogenic air separation unit on site, and the steam is partially produced as a by-product of cooling processes and partially from boilers at the facility. In addition to the formation of carbon monoxide and hydrogen, carbon dioxide, hydrocarbon

FIGURE 15-4 The Great Plains Gasi®cation Facility in Beulah, North Dakota, for the generation of methane from coal. The gasi®cation facility is in the foreground. Electricity is generated from the coal ®nes, which are not suitable for methane synthesis, in the power plant shown in the background next to the large smokestack. Photograph provided by Fred Stern at GPGF.

700

15.3 FOSSIL FUELS

gases, H2 S, NH3 , and ash are formed. The heat from this process volatilizes phenols, tars, and oil from the coal, which are collected as separate fractions. A portion of the carbon monoxide is further reacted with water to produce additional hydrogen [ (``shift reaction'': equation (6-10) ] so that there is suf®cient hydrogen to convert the remaining carbon monoxide to methane in the ®nal synthesis reaction [equation (6-12) ]. After cleanup of this raw gas to remove carbon dioxide, sulfur compounds, and light hydrocarbons, the ®nal synthesis of methane is carried out. Finally, water is removed from the gas to yield methane suitable for pipeline transportation and use as an energy source. The methane from this facility, 160 million cubic feet a day, is shipped by pipeline to the Midwest. The cost of producing methane in this facility is signi®cantly higher than the cost of obtaining methane from gas wells. Therefore the current focus is on the sale of the by-products to ensure that the overall process remains economically viable. Originally about 10% of the income for the facility came from the sale of these by-products, and the goal is to eventually have these compounds provide more income than the sale of methane. The hydrogen sul®de together with the waste light hydrocarbons is burned in the boilers and combined with the ammonia in a ¯ue gas desulfurization unit to produce ammonium sulfate, which is sold as DakSul 45 fertilizer. The remainder of the ammonia is stored in lique®ed form and sold. Some of the hydrocarbons and oils formed are used as an energy source at the facility, while the carbon dioxide is used for the enhanced recovery of oil from oil wells. Liquid carbon dioxide dissolves in some petroleum, thus increasing its volume and reducing its viscosity so that it ¯ows more readily. Carbon dioxide is not soluble in heavy oil so its main function is to displace the heavy oil to a location near the pipe used to remove the oil from the ground. Analysis of the phenolic fraction distilled from the lignite during gasi®cation revealed the presence of phenol and alkylated phenols. Currently the gasi®cation facility in Beulah is exploring methods for the separation of these compounds from tars to obtain catechols, which can be sold as starting materials for the synthesis of pesticides, dyes, and pharmaceuticals. In addition, the by-products from the cryogenic separation of oxygen have been found to have commercial value. These include nitrogen, argon, krypton, and xenon. Some of the liquid nitrogen is now being sold and some is used at the site. Krypton and xenon are now being sold while the economics for other gases, such as argon, is being explored. The direction of the research at this facility suggests that the key to the utilization of coal as an energy source may be to focus on the valuable byproducts formed in addition to the production of a clean liquid or gaseous fuel. It probably will not be possible to come up with one process for all facilities because the by-products will be strongly dependent on the source of the coal used and the type of gasi®er employed. For example, some of the features the

701

15. ENERGY

Great Plains facility tried to adopt from the SASOL process of South Africa did not work as anticipated, presumably because of the different grade of coal used.

15.4 NUCLEAR ENERGY 15.4.1 Nuclear Power and the Environment The discussion of nuclear energy in this chapter is limited to the established use of nuclear ®ssion to generate electricity in central station power plants. Weapons-related use is summarized in Chapter 14. Although nuclear power plants (NPPs) do not release the atmospheric pollutants that are emitted by fossil fuel power plants and are associated with the ``greenhouse effect'' and acid rain, some of their ef¯uents contain radionuclides and are, therefore, of environmental concern. Nuclear power plants are designed to be very nearly closed systems with respect to release of radioactivity into the environment during normal operation. They may release small amounts of ®ssion products and neutron-activated radionuclides. In the United States, the quantities released into the environment are legally limited by the regulations of the Nuclear Regulatory Commission (NRC), which licenses NPPs. To prevent release of radionuclides into the environment if there is an accidental loss of coolant (e.g., pump failure or break in the piping) in an NPP with an LWR7 steam generator, there is an emergency cooling system designed to prevent melting of the fuel rods and release of ®ssion products, uranium and plutonium. If the emergency system fails, escape of radionuclides is prevented by a physical barrier. The reactor and plant components that could contain radioactivity originating in the core of the reactor plant are enclosed in a steel-lined, reinforced concrete, single or double containment vessel (or structure or enclosure or building). The special enclosure also protects the reactor from damage from external forces. Both nuclear and fossil fuel power plants cause thermal pollution by transferring unused heat into the environment. Nuclear plants reject about 66% of the available heat; fossil fuel plants using steam turbines, about 60%. 15.4.2 Status of Nuclear Power 15.4.2.1 Worldwide

The ®rst central station power plant for the generation of electricity with ®ssion energy began operation in 1954 in the former Soviet Union. The 7

A light water reactor (LWR) is one that is moderated and cooled by H2 O.

702

15.4 NUCLEAR ENERGY

3000

Billion kilowatthours

2500 2000

Worlda

1500 1000

United States 500 0

1975 aEastern

1980

1985 Year

1990

1995

Europe and the former USSR are included beginning in 1992.

FIGURE 15-5 World and U.S. nuclear electricity gross generation, 1973±1999. Adapted from Monthly Energy Review, Section 10, January 2001. Energy Information Administration, U. S. Department of Energy, Washington, DC. http://www.eia.doe.gov/mer.

world nuclear electricity gross generation 1973 through 1999 is shown in Figure 15-5. The U.S. gross generation is shown for comparison. Countries that had one or more nuclear power plants at the end of 2000 are listed together with the total number of plants in Table 15-2. About 435 were in operation. Table 15-3 shows the nuclear share of total net electricity generated at the end of 1999 and estimated values for the year 2010 for countries that are members of the Organization for Economic Co-operation and Development (OECD).8 Prediction of the worldwide nuclear generation of electricity in, say, 20 years cannot be made simply by predicting the demand for electricity in each country, because nuclear power has become a politically divisive issue in many countries, including the United States. For example, Italy has phased out nuclear power, and Belgium, Germany, the Netherlands, and Sweden have made political decisions to phase out nuclear power. When this decision was made in Germany in June 2001, it was assumed that energy conservation, renewable energy sources, and importation of electrical energy from other countries would replace nuclear energy by the time all nuclear power plants are phased outÐabout 2021. In the United States it is likely that several nuclear power plants will be retired even though their licenses (for 40 years) might be renewable for another 20 years. However, the number of new plants to be built in France, South Korea, 8

Net generation is the electricity available for distribution (i.e., gross minus that needed to operate the plant).

703

15. ENERGY

and Japan may approximately balance the number to be phased out worldwide. In countries where the nuclear power industry is growing, there is an increasing interest in small ( 300 MWe ) and medium-sized (300±700 MWe ) plants. There is also an interest in using small nuclear plants to eventually replace gas turbines in cogeneration plants and diesel engines on ships.

TABLE 15-2 Countries with Nuclear Power Plants at the End of 2000 Country

Total number

Argentina Armenia Belgium Brazil Bulgaria Canada China Czech Republic Finland France Germany Hungary India Iran Japan Lithuania Mexico Netherlands North Korea Pakistan Romania Russia Slovakia Slovenia South Africa South Korea Spain Sweden Switzerland Taiwan Ukraine United Kingdom United States

3 1 7 3 6 22 11 6 4 59 20 4 18 1 58 2 2 1 2 2 5 31 8 1 2 20 9 11 5 8 18 33 107

Source: World list of nuclear power plants, Nucl. News, (3) 44, 61 (2001). (Revised annually.)

704

15.4 NUCLEAR ENERGY

TABLE 15-3 Nuclear Share of Total Electricity Generated (net TWh) in OECD Countries at the End of 1999 and Estimated Share for the Year 2010 Share (%) Country

Belgium Canada Czech Republic Finland France Germany Hungary Japan Korea (South) Mexico Netherlands Spain Sweden Switzerland Turkey United Kingdom United States

At end of 1999

Estimated for 2010

57.7 12.4 18.2 32.8 75.0 34.8 37.9 37.5 43.1 5.8 4.0 29.0 45.5 36.0 0.0 25.4 19.2

58.3 11.3 34.4 23.3 75.3 34.3 32.0 45.4 39.9 2.9 0.0 23.9 42.8 30.0 3.6 13.1 14.6

Source: Nuclear Energy Data 2000, Nuclear Energy Agency, Organization for Economic Co-operation and Development, OECD Publications, 2 rue AndreÂPascal, 75775 Paris Cedex 16, France (OECD Washington Center, 2001 L Street N W., Suite 650, Washington, DC 20036±4922).

15.4.2.2 United States

In the 1950s and 1960s, nuclear power was seen as the least expensive, most reliable way for the country's electric utilities to meet the projected annual increase in demand for electricity of about 7.5% in the 1970s, 1980s, and beyond. However, an abrupt change in projected demand for electricity in the United States followed the oil crises in 1973 and 1978. Energy utilization not only of oil but also of all energy sources was lowered signi®cantly by conservation and by improved ef®ciency of automobiles, appliances, and so on. As a result, the annual rate of increase in demand for electricity in the subsequent years dropped to less than 3.0%. It is expected that the annual increase in demand and replacement of aging central station power plants in the future will be met by gas-turbine plants fueled with natural gas. A full explanation of why no new nuclear power plants have been ordered in the United States since 1978 must go beyond the unexpectedly low increase in demand for electricity in the future. Factors contributing to this situation include safety, waste disposal, and the cost of generating electricity. Before a

705

15. ENERGY

Number of units

125 100

Peak: 122 units in 1990

75

104 units in 1999

50 25

42 units in 1973

0 1973 1975 1977 1979 1981 1983 1985 1987 1989 1991 1993 1995 1997 1999 Year

FIGURE 15-6 Number of operating nuclear power plants in the United States 1973±1999. From Monthly Energy Review, Section 8, January 2001. Energy Information Administration, U. S. Department of Energy, Washington, DC. http://www.eia.doe.gov/mer.

supplier of electric power will be willing to order a new nuclear power plant, the third of these factors must be favorable relative to that for new fossil-fueled plants that are being built and are scheduled to be built. The majority of these are relatively ef®cient plants that burn natural gas. Even if generating costs are favorable, a proposed NPP might never be built because of public opposition based on the ®rst two factors. In discussions of new NPPs in the United States it is usually assumed that such plants would be advanced BWRs or PWRs. However, a very different type of nuclear power plant that uses a gas-cooled, pebble bed modular reactor (PBMR) (see Section 14.7.4.4) has been receiving publicity as an alternative. If a proposed prototype (demonstration) plant is built (in South Africa) and is operated successfully, the safety characteristics of such a plant can be tested and the cost of generating electricity can then be estimated. Growth and decline of the number of NPP units operating in the United States from 1973 through 1999 are represented in Figure 15-6. Figure 15-7 illustrates the relative contribution of nuclear power to the total for the same period of time. A comparison of energy production from various sources is presented later (Figure 15-18). 15.4.3 Factors Affecting the Choice of Nuclear Energy for the Generation of Electricity in the United States 15.4.3.1 Availability of Other Energy Sources

The United States is fortunate in having fossil fuel resources and wellestablished technologies for their use. A number of industrialized nations (e.g., France, Japan, and South Korea) that lack such resources depend heavily on

706

15.4 NUCLEAR ENERGY

Trillion kilowatthours

4.0 Total

3.0

2.0

1.0

Nuclear electric power

0 1975

1980

1985 Year

1990

1995

FIGURE 15-7 Total and nuclear net electricity generation in the United States, 1973±1999. Adapted from Monthly Energy Review, Section 8, January 2001. Energy Information Administration, U. S. Department of Energy, Washington, DC. http://www.eia.doe.gov/mer.

nuclear energy to meet their present energy needs. They have, in fact, supported the development of fast breeder reactors, because such reactors convert the relatively abundant, non®ssile 238 U into ®ssile 239 Pu and have the potential of providing long-term energy independence. However, the availability of 235 U (after dilution with 238 U) and 239 Pu (after dilution with 238 U to form MOX (see Section 14.7.2) contained in the post±Cold War nuclear weapons stockpiles as fuel for NPPs has reduced somewhat the urgency for developing fast, liquidmetal-cooled breeder reactors. On the other hand, India, which has an abundant supply of monazite sand containing thorium but little uranium, is developing power reactors, including fast breeder reactors, which use the thorium fuel cycle (Sections 13.6.3 and 14.7.2) with 233 U as the fuel. 15.4.3.2 Safety

Prior to the Three Mile Island accident in March 1979 (Section 14.16.2.2), there had been numerous ``close calls'' or near accidents at NPPs. The TMI accident, together with the well-established association of nuclear power with the ``atom bomb,'' escalated uneasiness to fear, which generated an enduring negative reaction to nuclear power among the population in the United States and elsewhere. This fear of anything nuclear, exacerbated by the Chernobyl accident, was an expression of lack of con®dence in those responsible for safe operation of NPPs. However, since the TMI accident a steady effort has been

707

15. ENERGY

made in the United States by the nuclear power industry, the Nuclear Regulatory Commission through its regulations and inspections, and other safety organizations providing education and training to improve the safety record of nuclear power plants. In general, the effort has been successful and is perceived to have made nuclear power somewhat more acceptable to the public. 15.4.3.3 Fuel and Spent Fuel

Table 15-4 shows the unit energy content of coal, natural gas, oil, and uranium-235, as well as the quantities of fossil fuels that are equivalent in thermal energy content to one kilogram of uranium-235. Nonnuclear power plants that burn oil or natural gas have no spent fuel disposal problem. Spent fuel from a NPP is highly radioactive and requires safe storage at the plant site or at a temporary storage site until it can be taken to a geological repository for disposal as high-level radioactive waste. Although ash from a coal-®red plant contains chemical components of environmental concern (Section 6.9.1), its disposal is less challenging than that of nuclear fuel. However, spent nuclear fuel is discharged from the reactor less frequently (e.g., once in 12 months to once in 24 months).

15.4.4 Costs When the nuclear power industry was created in the United States, it was predicted that the cost of electricity to the consumer would be negligible. This seemed reasonable based on the cost of nuclear fuel. In reality, of course, the cost per kilowatt-hour of electricity delivered to the power transmission system

TABLE 15-4 Unit Energy Values for Fuels and Quantities of Fossil Fuels with Thermal Energy Content Equal to That of One Kilogram of 235 U Unit energy contenta Fuel

Equivalent energy content SI units

235 b U Coalc

82 TJ=kg 30 MJ=kg

Oil Natural gas

39 GJ=m3 38 MJ=m3

a

Btu 35 GBtu=lb 12.9 kBtu=lb 5.8 MBtu=bbl 1:02  103 Btu=ft3

1 kg 2:73  106 metric tons 2:13  103 m3 2:16  106 m3

1 Btu ˆ 1British thermal unit ˆ 1:054 kJ; 1 bbl ˆ 1 barrel ˆ 42 gal…U:S:† ˆ 0:159 m3 . for 239 Pu and 233 U are essentially the same as that for 235 U. Unit energy varies from 14 MJ=kg for lignite to 35 MJ=kg for bituminous coal.

b Values c

708

15.4 NUCLEAR ENERGY

by any type of central station power plant involves many costs in addition to that for fuel. 15.4.4.1 Capital

Nuclear power plants are more complex and, therefore, take longer and are more expensive to build than other plants having the same generating capacity. In addition to the reactor, safety-related construction costs such as those for the reactor vessel, the containment structure, the emergency cooling system, and temporary storage facilities for spent fuel are among the many costs that are unique for NPPs. Capital carrying charges for construction of a plant increase as the construction time increases. Construction time for nuclear power plants in the United States increased from an average of about 6 years prior to 1979 to an average of 11 years (with an upper value of 19 years) by 1989. By contrast, construction times have been about 6 years in France and South Korea and as low as about 4 years in Japan. One reason for increased construction time in the United States was delay caused by litigation9 brought by antinuclear groups and by others with the NIMBY (not in my backyard) philosophy. A second reason was delay resulting from design changes that were made during construction to ensure that the plant would meet new licensing criteria that re¯ected new safety features required by the NRC. Similarly, retro®tting new safety features into existing plants raised capital costs. Construction costs (adjusted for in¯ation) for a NPP in the United States increased from an average of about $800=kWe of generating capacity in the early 1970s to as high as about $3000=kWe for a plant at the end of the growth period 20 years later. It is expected that the new modular LWR plants that are precerti®ed by the NRC will take 5 or 6 years to build and will have construction costs estimated to be between $1000=kWe and $1700=kWe. It is very likely that if modular reactors are built, they would be placed on the sites of existing NPPs. Capital charges are estimated to be about 81% of the total cost for generating electricity for a new NPP, about 73% for a coal-®red plant, and about 28% for gas turbine plants. 15.4.4.2 Fuel

The contribution of fuel to the total cost is about 8% for NPPs, about 18% for plants burning coal, and about 67% for gas turbine plants. 15.4.4.3 Operation and Maintenance (O & M)

Compared with a fossil-fueled plant, a nuclear plant has very different control and operating characteristics and requires specially trained operating and maintenance personnel. Furthermore, the decay heat that is released after 9

The cost of the litigation itself adds to the total cost.

709

15. ENERGY

shutdown makes operation of a power reactor uniquely different from any other steam supply. The percentage of total generating cost stemming from O & M is about 11% for NPPs, about 10% for coal-burning plants, and about 5% for gas turbine plants. When an LWR power plant requires refueling, it must be shut down. During the scheduled shutdown (outage), maintenance work is performed. By 1999 the outages for some plants had been reduced from about 120 days to less than 20 days. In addition, the frequency of unplanned shutdowns has been reduced so that most plants are operating above 88% of annual capacity and some are at 100%. As a means of improving operation and lowering operating and maintenance costs for existing plants, a number of utilities have arranged to have their nuclear power plants either operated by or purchased by companies that specialize in the management and operation of nuclear power plants. Some utilities have merged and others have combined to form joint operating companies for their nuclear power plants in order to make them more competitive. These efforts to reduce O & M costs for well-operated NPPs in the United States have succeeded in bringing the average cost of electricity down suf®ciently to be competitive with plants fueled with coal. The presence of ionizing radiation makes maintenance of certain regions of a nuclear power plant dif®cult and expensive. The requisite radiation safety program for monitoring plant workers adds to the operating cost of a nuclear power plant. A number of utilities have been ®ned heavily by the NRC because of operational safety problems. In general, safety of operation has greatly improved over the years. For example, the collective exposure to ionizing radiation of plant workers is about 80% lower than it was two decades ago. 15.4.4.4 Decommissioning

When an NPP ceases to operate and is decommissioned, it can be mothballed temporarily or it can be dismantled immediately, decontaminated, and the buildings put to other use or demolished to provide a ``green ®eld'' site. Whenever an NPP is dismantled, a large volume of radioactively contaminated structural material and equipment is generated. The rate that the owner of an NPP charges its customers for electricity includes an amount that is accumulated in a decommissioning fund during the lifetime of each of its nuclear power plants. 15.4.4.5 Other

Also included in the cost of operation of a nuclear power plant are (1) a security program to protect the plant from intruders including terrorists and (2) a safeguard and accountability program to assure that the plutonium produced in the plant is not accessible for use as a weapons material or as a radiotoxic contaminant.

710

15.5 SOLAR ENERGY

15.5 SOLAR ENERGY 15.5.1 Introduction Although only about 2  10 9 of the radiation from the sun reaches the earth, sunlight represents a tremendous source of renewable, greenhouse-gas-free energy. We saw in Chapter 3 that the solar constant, which is the average solar energy ¯ux (i.e., solar power) of all wavelengths at the top of the atmosphere, is about 1:37 kW=m2 . This corresponds in one second to 1:37 kJ=m2 of energy. Commercially, energy is often expressed in terms of kilowatt-hours, or kWh, which is the amount of power in kilowatts provided or produced over a time period of one hour. Thus, the amount of energy from the sun at the upper edge of the earth's atmosphere is 1:37 kWh=m2 in one hour, or in one year (8760 hours), 12:0 MWh=m2 …1 MW ˆ 1000 kW†. Not all this energy is available at all times at a given site on the earth's surface, however. For one thing, it varies diurnallyÐfrom day to night over a 24hour periodÐas the earth rotates. We have also seen that much of the sun's radiation (particularly in the ultraviolet and infrared spectral regions) is absorbed in the atmosphere, so that most of the radiation reaching the biosphere is in the visible region. Of this, about 30% (the earth's albedo) is re¯ected back to space. The amount impinging on one square meter of the earth's surface also varies seasonally and with the latitude. Figure 15-8 shows the annual average available solar energy across the United States, using a collector that can be rotated to keep it perpendicular to the sun's rays, ranging from 3:6 MWhm 2 y 1 at Las Vegas to 1:8 MWhm 2 y 2 at Seattle. Assuming a national average of 2:1 MWhm 2 y 1 , this amounts to approximately 2:1  1013 MWh=y of solar energy for the whole country (1013 m2 ), or about 1000 times the energy consumed by the United States.10 There are several important ways that solar energy may be directly utilized, and these are covered in this section. It should also be pointed out that although wind and water are reviewed in a separate section (Section 15.7), the ultimate source of these energies is also of course solar energy. These energy sources are renewable, in contrast to fossil and even nuclear fuel sources. Table 15.5 at the end of Section 15.7.3.3 gives a summary comparison of most of them. Available sunlight is both direct and diffuse; that is, some of the sun's radiation comes directly from the sun, while the rest of it reaches the earth's surface indirectly by atmospheric scattering or refracting. (The total of the two is called global.) On very clear, cloudless days the direct sunlight may make up 10 In 1990 the United States consumed 2:4  1013 kWh (82 quads) of energy, which was 24% of the whole world's use of about 1014 kWh that year. By the year 2026 the annual world energy use is predicted to increase by about 50%.

711

15. ENERGY

Megawatt-hours per square meter 1.6−1.8 1.8−2.2 2.2−2.6 2.6−3.0 3.0−3.4 3.4–3.8

FIGURE 15-8 Average annual solar radiation in the United States. From K. Zweibel, ``Harnessing Solar Energy,'' p. 220. Plenum Press, NY, 1990.

as much as 90% of the total solar radiation, whereas on very cloudy days 100% of the available sunlight may be diffuse. Utilization of the two components of sunlight depends on the technique being employed. Diffuse light produces ``low-grade'' energy, which can be used, for example, for solar heating. However, production of ``high-grade'' energy, such as conversion directly to electrical energy with photovoltaic cells, in general requires direct sunlight. Probably the most effective uses of solar energy will involve simultaneous integration of technologies, such as the hybrid units of photovoltaic and solar thermal energy cells currently being developed.

15.5.2 Biological Utilization of Solar Energy: Biomass In its broadest sense, biomass (living matter) is the earth's vegetationÐthat is, plant material produced by photosynthesis, with the result that solar energy is stored.11 This encompasses agricultural crops, forests, grasslands and savannas, and so on. The overall equation of oxygen-producing photosynthesis is 11 Photosynthesis is the process by which green plants, algae, and some bacteria convert light energy to chemical energy to sustain their life. It has existed in its present form for at least 3.5 billion years, and undoubtedly it is the most important photoprocess occurring in nature. Since all the earth's coal and oil deposits come from past photosynthesis, all our food and most of our fuels are products of this process.

712

15.5 SOLAR ENERGY

light

CO2 ‡ H2 O !

1 …CH2 O†n ‡ O2 n

…15-7†

in which …CH2 O†n represents any carbohydrate, including sugars, starches, and lignocellulose. Biomass has been used for many centuries for heating, lighting, and cooking. It is still the primary source of energy for half the world's population and produces 13% of the world's energy, but in the developed industrial countries fossil fuels have been much more widely used for many years.12 The use of biomass for the generation of electric power, which historically has been used primarily by the paper and wood products industries utilizing waste wood fuel, is expected to increase in the United States from approximately 10 GW in 1997 (about 2% of the total U.S. generating capacity) to more than 100 GW by the year 2030. In addition, there are wellestablished methods for producing liquid (biofuels) and gaseous (biogas) fuels from biomass (Chapter 6). Brazil, for example, has developed an extensive fuel program for production of ethanol from sugarcane: in 1995, 35% of the passenger cars in Brazil were fueled with pure ethanol, the remainder using blended fuels containing 22% ethanol. An 85% ethanol (15% gasoline) fuel is being marketed in the United States for use in automobiles designed to run on it and on 100% gasoline. We see by reaction (15-7) that photosynthesis uses up CO2 ; therefore, biomass is an important ``sink'' for this primary ``greenhouse gas'' (see Chapter 3). It follows, then, that the ongoing destruction of tropical forests, in which photosynthesis is a major naturally occurring reaction, is one of the major contributors to enhanced global warming. One way of moderating the current increase in atmospheric CO2 might be to develop extensive new forests. However, uptake and storage of CO2 by trees greatly decreases as the trees mature, and even at that most of the trees will die and decay within a century or so if not harvested, releasing again the stored CO2 . In the long run it may be better to develop fast-growing biomass plantations for eventual CO2 -neutral energy replacement of fossil fuels rather than for limited-time CO2 reduction given by permanent forests. An example of such a process is short-rotation coppice (SRC). In this technique fast-growing young growth from woody biomass is harvested, and resprouting (coppicing) growth from the left-behind stumps is cultivated and reharvested. SRC can produce high yields of biomass in a relatively short timeÐup to about 10 yearsÐon a sustainable basis. It needs to be emphasized, however, that biomass fuel will be completely CO2 neutral only if no nonrenewable energy sources are used in all stages of production, processing, and distribution. This will not be the case in the foreseeable future. For example, fossil fuels are extensively used in the manufacture of nitrogen fertilizers and in transportation. Furthermore, biomass use 12

However, in the United States biomass is nevertheless the second largest renewable energy source (after hydroelectric power: see Section 15.7.3.1).

713

15. ENERGY

will make sense only if there is an overall net positive energy balance,13 and processes such as the production of nitrogen fertilizers are very energy intensive. It is estimated, for example, that the net energy balance for the production of ethanol from wheat, a cultivated crop grown from seed, either is negative or has a low positive energy balance (between 1.0 and 1.2). On the other hand, energy balances for SRC may be positive by at least an order of magnitude. It is also worth noting that biomass is generally lower in sulfur than most coals. This may be an important bene®t of biomass in view of recent regulations in some countries reducing SO2 emissions by electric power utilities. There are, however, several serious environmental concerns with use of biomass as a major renewable energy source. Intensive agricultural practices often lead to nitri®cation of water supplies and pesticide and herbicide residues. Major production of biomass for energy usage will also require large land area commitments. For example, it is estimated by the U.S. Department of Energy that about 100 mi2 (25,000 hectares) of land will be required for an advanced 150-MW biomass power plant, which means that approximately 70,000 mi2 (about 2% of the total land area of the country) will be needed to meet the above estimate of 100 GW of electrical power from biomass by 2030 if there are no major increases in biomass productivity. Some major agricultural areas in developed countries can produce far more food than is needed by their residents, and biomass growth for energy purposes may lead to more effective use of productive but uncultivated land. For some developing countries, however, emphasis on biomass production could lead to intense competition between land and water use for food and for biomass energy production.

15.5.3 Physical Utilization of Solar Energy 15.5.3.1 Solar Heating and Cooling

About 20% of all the energy consumed in the United States goes for domestic hot water and for heating and cooling of buildings. Solar heaters to provide domestic hot water for homes and residential buildings have been commercially available in countries such as Japan and Israel for many years. Following the 1973 oil embargo (Section 15-1), a large number of electric utilities initiated major research and development programs in solar heating and cooling; these have involved literally thousands of experimental and developmental installations demonstrating energy conservation as well as utilization of 13 Net energy balance is a measure of the difference between the energy contained in the biomass fuel and the total energy required to grow, harvest, and process the crops used in its production. Often the net energy balance is expressed (as we will do here) as a ratio of these two quantities (i.e., the energy contained in the biomass fuel divided by the total energy used in its production).

714

15.5 SOLAR ENERGY

solar energy. The renewal of an abundance of low-cost oil led to a decrease in this activity by utilities since the early 1980s. Nevertheless, at this time the space heating and cooling of buildings is probably the most developed direct usage of solar energy, although hydroelectric power, which is a form of solar energy utilization (see Section 15.7.3.1), generates much more energy than is converted to thermal energy by solar energy collectors. Since this is lowtemperature energy usage, it readily lends itself to utilization of solar energy, and the basic technology is available now. Homes and buildings with roof solar collectors for domestic hot water are now common sights, particularly in regions of high and extensive sunshine such as the southwestern United States. Solar heating and cooling may be divided into two categories: passive and active. Passive systems use only natural conduction, convection, radiation, and evaporation, while active (nonpassive or hybrid) systems employ external energy to run fans, solar circulating pumps, water pumps, and so on. The early active systems were quite complex and unreliable, and the trend in recent years has been toward simplicity in passive and hybrid systems that use minimal nonrenewable energy sources. In most locations the installation and maintenance costs of active systems still substantially exceed the energy cost savings, but passive systems are cost-effective in many areas. A typical procedure is to use a solar collector to absorb the solar energy, converting it to thermal energy, which is transferred by heat pipes or pumped ¯uids directly for low-temperature ( 1008C) heating or for storage. The collector should therefore have high thermal conductivity and low thermal capacity, such as metals (copper, steel, and aluminum) and some thermalconducting plastics. The most common collectors are ¯at blackened plates, since they convert both direct and diffuse (cloudy) solar radiation into heat. Heat losses from collectors result mainly from re¯ection, thermal (blackbody) emission (Section 3.1.1), and convection. Re¯ection and thermal emission losses can be reduced by selective surface coatings, and convection losses are reduced by covering, or glazing, the front of the collector with a glass that transmits most of the radiation but traps the convection heat between the absorber and the glazing, and by insulating the back side of the collector. (Further reduction in convection lossÐalmost to zeroÐis attainable by evacuating the space between the collector and the glazing, but such collectors can be very expensive to manufacture and maintain.) In many cases (up to 1008C), water is the heat transfer ¯uid. Liquids with high speci®c heats (such as mineral oils and glycols) are employed at higher temperatures, however, and at very high temperatures molten salts or liquid sodium are used. Although it is best to use the converted solar energy directly, sunlight is intermittent. Thus storage of the converted thermal energy is a very important factor in its ef®cient and economical utilization. Several large-scale energy storage techniques are covered in Section 15.8. However, heat can be stored for several days by sensible (speci®c) heat storage using water or other ¯uids in

15. ENERGY

715

insulated tanks or rocks (pebble bed) for gas, and by latent heat storage with phase-change materials.14 Materials used for latent heat storage are generally more expensive than those used for sensible heat storage but have a much higher density for energy storage. For example, calcium chloride hexahydrate (CaCl2
6H2 O) is extensively used as a phase-change material involving its latent heat of fusion (melting); it melts at about 278C, has high thermal stability, and can store 2:8  105 kJ=m3 . By comparison, water would have to be heated about 678C to store as sensible heat an equivalent amount of thermal energy stored as latent heat by CaCl2
6H2 O for the same volume. Direct (but only a small fraction of diffuse) solar radiation can be concentrated by re¯ecting light with an array of mirrors (a heliostat) onto a common collector. Heat losses are minimized because the surface area of the absorber can be relatively small, and very high temperatures are possible. An extreme example is the experimental High Flux Solar Furnace built in 1989 at the National Renewable Energy Laboratory (NREL) in Colorado, in which the intensity absorbed by the collector furnace, using a series of focused heliostats, is equivalent to 50,000 times the intensity of direct (unfocused) sunlight, generating temperatures up to 30008C. We will see in Section 15.5.3.2 that this technique is extensively used in solar thermal electric power systems. Solar air conditioning, although not as well developed as solar heating, has the advantage that it is most needed on hot sunny days when solar radiation is also plentiful, particularly in commercial buildings, where less air conditioning may be needed at night. There are two main solar air conditioning systems currently in use involving cycles based on the very old technique of evaporative cooling; these are the absorption cooling system and the desiccant cooling system. Figure 15-9 is a very simpli®ed schematic drawing of an open-cycle absorption cooling system. Liquid water, the refrigerant,15 is added to the system at the evaporator, where the pressure is reduced and the water is ¯ash-vaporized. This results in the absorption of heatÐthe latent heat of vaporization of the waterÐhence removal of heat (via a heat-exchanger coolant) from the space to be cooled. The water vapor is fed to the absorber, where the concentrated absorbent solution (often a lithium bromide solution) absorbs the water vapor and the heat evolved in this dilution process is discharged to the atmosphere. The diluted absorbent solution is pumped to the regenerator, where it is heated by solar light; this results in desorption of water and thus regeneration of the concentrated absorbent solution, completing the cycle. 14 Sensible heat storage involves heating up the material (with no phase change), the stored energy being released as the material is cooled. Latent heat storage involves a phase change that absorbs energy (e.g., melting a solid) and releases the energy when the phase-change process is reversed (solidi®cation). 15 In the open-cycle system, water is almost always used as the refrigerant; it is continuously fed into the system and discharged to the atmosphere after being used for cooling. In a closed-cycle absorption cooling system, the refrigerant is reused in subsequent cycles.

716

15.5 SOLAR ENERGY

Sunlight

Regenerator Concentrated absorbent solution Heat discharged to atmosphere

Water vapor to atmosphere

Diluted absorbent solution Low-pressure water vapor Absorber

Liquid water

Evaporator

Heat removed from space to be cooled

FIGURE 15-9 Simpli®ed schematic of an open-cycle absorption cooling system using water as the refrigerant. Modi®ed from M. Wahlig, ``Absorption Systems and Components,'' in Active Solar Systems, G. LoÈf, ed. The MIT Press, Cambridge, MA, 1993.

Similarly, in the open-cycle desiccant cooling system ambient air is dried by blowing it over a solid desiccant such as silica gel or a molecular sieve, or a liquid desiccant such as glycol is circulated through the airstream; in either case the air heats up because heat is given off when water is removed by a desiccant. The hot, dry air is then cooled by passing it through a heat exchanger and by evaporating water into it similar to the absorption cooling system, with the desiccant being regenerated with outside air warmed by solar heating. Both systems permit independent control of humidity and temperature. In general, the initial cost of either a solar heating or cooling system alone is so great that they are not economically feasible and cannot be justi®ed for seasonal operation only. Since much of the solar energy collecting and recycling equipment can be common to both systems, however, combined heating± cooling systems may make this form of solar utilization viable; even greater economies may be realized if the solar units can also be used to supply domestic hot water to the buildings being heated or cooled. 15.5.3.2 Solar Thermal Electric Power

Solar thermal electric power is generated by converting solar energy ®rst into heat and then into electric power, generally by steam-generating techniques similar to those used in conventional power plants where the source of heat is a gas-, coal-, oil-, or nuclear-®red furnace. As with solar heating and cooling, major solar thermal electric power research and development programs evolved after the oil shortage of the early 1970s, only to decline in the 1980s after world oil prices dropped and long-term, low-cost electricity seemed assured. Nevertheless, this technology has the potential to provide an important renewable energy supply in the future.

717

15. ENERGY

Conversion to thermal energy is an intermediate step in the conversion of solar energy to electrical energy, in contrast to direct conversion as with photovoltaic or photoelectric utilization (see Sections 15.5.4 and 15.5.5). Therefore the fundamental thermodynamic second-law limitation (Section 15.2.1) on the ef®ciency of the process applies. We see by equation (15-5) that the greater the temperature difference, the greater the ef®ciency of the energy conversion, hence the need in most cases of solar thermal electric technology to use a high-temperature solar heat source. (One exception to this is the use of solar ponds for electric generation; see Section 15.5.3.3.) This requires focusing direct sunlight onto a collector, similar in principle to the technique just described in connection with solar heating (Section 15.5.3.1). There are three basic methods used for this: the central receiver, the parabolic dish, and the parabolic trough. All three systems eventually convert re¯ected sunlight into thermal energy, which is transported by a heat transport ¯uid (water=steam, molten salts, or liquid sodium) to a central location for thermalto-electric energy conversion or for energy storage as sensible heat. The central receiver system uses a single tower-mounted receiver to collect focused, re¯ected sunlight from a large ®eld of assembled sun-tracking mirrors.16 Parabolic dish systems use a collection of point-focusing re¯ectors; each re¯ector tracks the sun in two axes and focuses the light onto a receiver at its focal point. Parabolic troughs are U-shaped (line-focusing) re¯ectors that re¯ect the sunlight onto a linear receiver located along the focal line of the trough. The parabolic trough system is the most fully developed of the three, and probably because of its lower operating temperatures, it is the most useful for industrial process heat applications. Several hybrid parabolic trough plants (also using natural gas) are now in commercial operation in California. However, the potential for future economic utilization of solar energy is greater for either the central receiver or the parabolic dish technology, although neither is technically feasible for commercial deployment now. 15.5.3.3 Solar Ponds

Hot water normally rises by convection and mixes with cooler water in a pond because above 48C the density of water decreases with increasing temperature. However, a temperature inversion can result if the pond is made nonconvective by some convection barrier. In a salt gradient solar pond, this is accomplished by establishing an increase in salt concentration (hence an increase in density) from top to bottom, so that the water is denser at the bottom than at the top even if the water at the bottom is heated by transmitted solar light to a 16 For example, a 10-MW central receiver demonstration solar power plant in the Mojave Desert (California) uses 2000 motorized mirrors to focus sunlight onto a receiver, heating to 5658C a molten nitrate salt that boils water to drive a steam electric turbine.

718

15.5 SOLAR ENERGY

relatively high temperature. Thus, solar ponds are a means for collecting direct solar energy and storing it as heat for low-temperature applications. Naturally occurring salt gradient ponds in Transylvania were ®rst studied in 1902, and this technique is currently being investigated in many countries for economically feasible collection and storage of solar energy. Considering only buoyancy, a salt gradient pond will be stableÐthat is, nonconvectiveÐas long as the salt concentration is high enough to compensate for thermal expansion. Since water in this state is not convective, it behaves as a thermal insulator, the only loss being by conduction. The largest temperature difference is between the surface and the bottom (which may be a difference of 40±508C), and thus most of the useful energy is in the lower regions of the pond. Actually most ponds do not have a continuous salt gradient, but rather at least three distinct zones or layers, as shown in Figure 15-10. The top (surface) and bottom (storage) zones frequently are of uniform concentration and therefore are convective within each one separately, but the middle (gradient) zone must have a concentration gradient and therefore be nonconvective.17 The concentration gradient is established by ®lling the solar pond with concentrated salt solution to a depth of the storage zone plus about half the gradient zone; fresh water is added to the solution at successively higher levels, creating the gradient, followed ®nally by adding a layer of fresh water on

Sunlight

Surface zone

Gradient zone Storage zone

Heat exchanger pipes FIGURE 15-10 Schematic diagram of a three-zone salt-gradient solar pond. 17 Advanced solar ponds have an additional strati®ed thermal layer consisting of several sublayers of different densities between the gradient and storage zones.

719

15. ENERGY

top, forming the surface zone. The ponds are lined with clay or a plastic membrane buried in clay to minimize heat loss to the earth and to prevent salt loss. Heat is extracted by placing heat exchanger pipes in the storage zone or by pumping brine from the storage zone to an external heat exchanger. (Heat can also be removed from the strati®ed thermal zone in an advanced solar pond.) As with most other solar energy utilization systems, solar ponds do not pose major environmental problems, although leaks or waste disposal procedures can lead to serious salt contamination. The energy gained per unit area of a solar pond is roughly the same as for a ¯at plate collector, and the pond has the additional advantage of having its own built-in energy storage. If reasonable sunlight and adequate low-cost supplies of water and salt are available, and if the land site can tolerate a large open pool of water, then a solar pond can provide low-temperature energy much more favorably than ¯at-plate collectors for many uses such as thermal heating and cooling, domestic hot water, desalination (distillation or electrodialysis), crop drying, and energy-intensive processes in hydrometallurgical mining (that is, the recovery of metals from ores by leaching with aqueous solutions). Also, although this is low-temperature thermal energy and therefore low ef®ciency for solar energy utilization, since it involves indirect conversion to electrical energy via thermal energy, it may turn out to be economical for electric power generation in areas where nonrenewable fuel costs are very high. An example is the electric power station at Beit Ha'Arava, Israel, at the north shore of the Dead Sea. This plant has been in operation since 1984, and uses a 40,000-m2 pond and a 210,000-m2 pond to operate a 5-MW power station. 15.5.3.4 Ocean Thermal Energy Conversion

The process called ocean thermal energy conversion (OTEC) converts thermal to mechanical to electrical energy by using the temperature difference between ocean surface waters that are warmed by absorption of solar energy and the colder waters at depths below 1000 m that come from Arctic regions. Generally the temperature difference DT even in the tropical and subtropical oceans is at best only about 208C, and it is estimated that this gives an overall operating energy ef®ciency of the order of 2%. Three systems have been studied for OTEC. In the closed-cycle system, Figure 15-11a, a low boiling working ¯uid such as ammonia is vaporized by the warm surface water and the working ¯uid vapor drives a turbine electric generator. The vapor is then condensed by the cool deep ocean water and the cycle is repeated. The working ¯uid in the open-cycle system (Figure 15-11b) is the warm surface ocean water itself. It is vaporized in a low-pressure ¯ash evaporator, and the vapor (steam) drives a low-pressure turbine. The steam is condensed by the cool water via a heat exchanger, producing desalinated

720

15.5 SOLAR ENERGY

Discharge deep water to ocean

Warm surface ocean water in Working fluid vapor

Evaporator

Turbine electric generator

Working fluid vapor

Discharge surface water to ocean Working fluid liquid

Condenser

Cool deep ocean water in Working fluid liquid

Pump (a)

Noncondensable gases Warm surface ocean water in

Low-pressure flash evaporator

Desalinated water vapor

Discharge deep water to ocean Desalinated Low-pressure water vapor turbine electric generator

Condenser

Desalinated water

Cool deep ocean water in

Discharge warm surface water to ocean

(b) FIGURE 15-11 Schematics of ocean thermal energy conversion (OTEC) systems. (a) Closedcycle system; (b) open-cycle system. Modi®ed from P. K. Takahashi and A. Trenka, Energy, , 657 (1992).

potable water suitable for human useÐa valuable by-product particularly in tropical locations with little available groundwater. In the hybrid system the low boiling working ¯uid that is used to generate electricity is vaporized at a heat exchanger by the water vapor from a low-pressure ¯ash evaporator, and the condensate is removed as desalinated water. There are other ``by-products'' of OTEC in addition to desalinated water. The cold water pumped up from the ocean depths is good for cultivation of marine organisms (mariculture) such as salmon, shell®sh, kelp, and other algae. It can also be used for refrigeration and air conditioning. Several OTEC systems of up to 500 kW have been demonstrated, and it is expected that the ®rst commercial units early in the twenty-®rst century will be in the 1- to 10-MW range. It is generally agreed that for OTEC to be economically viable, it will have to utilize its ``by-products'' of desalinated water and mariculture in addition to generating electricity.

721

15. ENERGY

15.5.4 Photovoltaic Utilization of Solar Energy The photovoltaic effect is the production of an electric potential and current when a system is exposed to light; a solar photovoltaic device or cell is one in which the light source is the sun. Since solar energy is converted directly into direct-current electricity without going through the intermediate conversion to thermal energy (heat), it is not restricted by the second-law ef®ciency limitation. The ®rst major impact of solar cells was in the 1950s in spacecraft, where reliable and long-lasting power supplies were essential but cost was not a signi®cant factor. Photovoltaic devices are currently the most promising systems for the direct conversion of sunlight into electrical energy. A solar cell is a semiconductor recti®erÐthat is, electric current ¯ows only in one direction. Figure 15-12a is a simpli®ed one-dimensional energy diagram based on the band model of solids, for a pure crystalline semiconductor at 0 K showing two allowed energy bandsÐa completely ®lled band, the valence band, and a completely empty band, the conduction bandÐseparated by a forbidden zone, the band gap Eg . (The vacuum level is the energy of an electron at rest in a vacuum.) At room temperature, however, some electrons (e ) in the semiconductor valence band are thermally excited into the conduction band, leaving behind a vacancy or positive ``hole'' (h‡ ) in the valence band, as shown in Figure 15-12b. This formation of an electron±hole pair results in the small amount of room temperature conductivity characteristic of a semiconductor.18 Addition of a very small amount (as little as 10 6 mole fraction) of an appropriate impurity greatly increases the conductivity of a semiconductor; this is called doping. A p-type (positive) semiconductor is a material doped with atoms having fewer valence electrons than the semiconductor material; these are called acceptor atoms. For example, boron has three valence electrons, one less than silicon.19 Thus if B replaces a silicon atom in a crystal, there is an electron vacancy (or a positive hole, h‡ ) in the valence band. On the other hand, if a silicon atom is replaced by a phosphorus atom (a donor atom) with ®ve valence electrons, there is an extra electron, which must occupy the conduction band; this is called an ``n-type'' (negative) semiconductor.20 18

Like semiconductors, insulators also have completely ®lled valence bands and completely empty conduction bands at 0 K; they differ from semiconductors in that even at room temperature electrons are not thermally excited into the conduction band of an insulator. (This is because insulators have larger band gaps than semiconductors.) The conduction bands of metals are partially ®lled even at 0 K. 19 Silicon (Si), the second most abundant element on earth, is the most studied and most used semiconductor material for solar cells in addition to its widespread use in the electronics industry. A large number of compound semiconductor materials (such as GaAs, CdTe, and CuInSe2 ) are also being extensively studied for use in thin-®lm solar cells. In general, however, material and production costs have so far made these economically unfeasible. 20 In either case the overall crystal remains neutral because the positive nuclear charge has also been changed by one unit.

722

15.5 SOLAR ENERGY

Vacuum level Conduction band ECB Eg EVB

Valence band

(a)

Vacuum level Conduction band e−

e−

ECB Eg EVB

h+

h+ Valence band

(b) FIGURE 15-12 Schematic energy diagrams for a pure crystalline semiconductor. (a) 0 K; (b) room temperature.

If now a p-type semiconductor and an n-type semiconductor are intimately joined, a pn-junction semiconductor is formed. Some of the conduction band electrons in the n side diffuse a very short distance into the p side, where they combine with holes, resulting in a layer of negatively charged acceptor atoms; at the same time some of the extra positive holes diffuse from the p side into

15. ENERGY

723

the n side and combine with electrons, giving a layer of positively charged donor atoms. This produces a double layer of charge, hence a built-in internal potential at the junction, the junction potential (Figure 15-13a).21 This permanent potential barrier, penetrable only by highly energetic electrons, is necessary to maintain the separation between the remaining weakly bound excess electrons in the n-type side and the excess holes in the p-type side.22 Most solar cells are pn-junction semiconductors. Generally they consist of a p-doped base coated on the front with a thin layer of n-doped material, producing the pn junction. On top of this is a metal grid for electrical contact that also serves as a window to allow a high percentage of the incident radiation to pass into the cell. The entire bottom is covered with a metal to provide the other electrical contact. When a photon with energy at least greater than the band gap Eg is absorbed by the semiconductor, an electron±hole pair can be formed with the electron excited into the conduction band, leaving behind the positive hole in the valence band, as shown in Figure 15-13b. The photoexcited electrons migrate preferentially to the n-type side and the photoproduced positive holes move toward the p-type side, regardless of the side of the pn junction on which the electronic transition takes place, making the ntype side negative with respect to the p-type side. This set of migrations produces the photopotential, so that if a wire is connected to the two sides, electrons will ¯ow in the external circuit from the n-type side to the p-type side.23 The ef®ciency of a solar cell is the percent of the incident sunlight power that is converted to electrical output power. In general the major factor limiting the ef®ciency is the amount of the solar spectrum utilized in the conversion, although recombination processes between electrons and holes that reduce the photocurrent may also be important depending on the types of semiconductors involved. For power usage, many individual monocrystalline solar cells are connected together to give a module, or amorphous or polycrystalline layers are deposited on a large surface such as glass or plastic or another semiconductor. These can be ¯at-plate modules to absorb low-intensity diffuse sunlight, or lenses and a tracking mechanism can be used to focus direct sunlight onto the cell.24 A group of connected modules is called an array. 21 It is assumed as an approximation that there are no charge carriers (neither electrons nor holes) in the depletion region. 22 There are other ways of generating a potential barrier in a semiconductor (e.g., the Schottky diode), which are, however, beyond the scope of this book. 23 However, only the photoproduced electrons and holes that cross the depletion region before they recombine contribute to this external current. 24 Concentrating the light also tends to increase the ef®ciency of solar cells at lower light intensities, up to concentrating ratios of from 20-fold to several hundredfold, but the cells must be kept cool because high temperatures reduce the ef®ciency.

724

15.5 SOLAR ENERGY

Vacuum level Junction potential Conduction band − − − − − − − − −

ECB

EVB

Depletion region

+ + + + + + + + +

Eg

Valence band p side

n side Junction (a) Sunlight

Vacuum level Conduction band

e−

e−

ECB

e−

e−

h+

h+

EVB

h+

h+

Valence band p side

n side Junction (b)

FIGURE 15-13 Schematic energy diagrams for an np-junction semiconductor. (Thermally excited electron-hole pairs not shown.) (a) Dark; (b) illuminated.

725

15. ENERGY

Many thousands of small stand-alone photovoltaic or hybrid (photovoltaic plus diesel) power systems are in use throughout the world. These provide power for applications such as water pumping, lighting and home power, telecommunications, and vaccine refrigeration, particularly in remote rural areas where in many cases this has become the least expensive method of electric power generation. Presumably, though, the most important impact of photovoltaic devices in addressing the energy requirements of the United States will be with large (up to gigawatt) plants for utility grid distribution. Many experimental and demonstration units for bulk power generation have been built around the world by public and private utilities. For example, the largest ever constructed to date was the 6.5 MW facility at Carissa Plains, California; completed in 1985, it has recently been dismantled. The largest rooftop solar power plant at this date is the 1-MW installation built in 1997 at the New Munich Trade Fair Center. The ®rst photovoltaic project attached directly to a utility power grid near where the electricity will be used (rather than centrally located and distributed to outlying areas as is traditionally done) is the 500 kW plant at Kerman, California that became operational in 1993. Experience has shown that utility-sized photovoltaic plants made up of many single-crystal silicon solar cell arrays providing megawatt power can operate reliably and with satisfactory performance. Several techniques appear to be close to economical feasibility, and when the relatively benign environmental impacts and the appreciable social bene®ts are considered, photovoltaic-generated utilityscale power is probably competitive with fossil fuel electricity even at the time of this writing.

15.5.5 Photoelectrochemical Utilization of Solar Energy 15.5.5.1 Electrochemical Photovoltaic Cells

We have seen that photovoltaic solar cells are essentially light-sensitive semiconductor recti®ers constructed of solid-state materials. Electrochemical photovoltaic cells, or photoelectrochemical cells, are similar to ordinary electrolytic cells except that one of the electrodes is a photosensitive semiconductor instead of a conducting metal. Irradiation of the semiconductor electrode converts solar energy to electric energy, generating a photoelectric current and potential in the external circuit. This may be the only effect if the oxidation±reduction (redox) reaction at one electrode is the opposite of that at the other electrode so that no overall reaction occurs; this is called a regenerative cell. On the other hand, solar energy may be stored as chemical energy (fuel) if electrolyte products are produced at one or both of the electrodes (a nonregenerative cell). An example of this latter effect, the photoelectrochemical production of hydrogen, is covered in Section 15.5.5.2.

726

15.5 SOLAR ENERGY

When a semiconductor electrode is immersed in an electrolyte, chargetransfer equilibration between the semiconductor and the electrolyte results in formation of a thin space-charge layer in the semiconductor near the surface that is in contact with the electrolyte. For n-type semiconductors with an excess of electrons (see Section 15.5.4), the equilibration reduces the concentration of the electrons within the space-charge layer, whereas for p-type semiconductors with a shortage of electrons (an excess of positive holes) the concentration of the positive holes is reduced. This produces a potential barrier analogous to the internal potential at a pn junction in a photovoltaic cell (Figure 15-13a); however, in a photoelectrochemical device the barrier is within the semiconductor just beneath the interface with the electrolyte rather than in the interface between the two solids as in a solid-state photovoltaic device. Shining light of photon energy equal to or greater than the band gap energy Eg of a photosensitive semiconductor again produces electron±hole pairs, exciting electrons from the valence band to the conduction band and leaving positively charged holes in the valence band. Thus, if an illuminated ntype semiconductor electrode is connected by the external circuit to an inert metal counter electrode and both are immersed in an appropriate reversible redox electrolyte, the holes migrate to the semiconductor surface, where they oxidize the reduced form of the redox electrolyte, and the electrons ¯ow through the external circuit to the counter electrode where the oxidized component of the redox electrolyte is reduced. Conversely, for p-type semiconductor electrodes the photoexcited electrons migrate to the redox electrolyte at the semiconductor surface, reducing the oxidized form, and the positive holes oxidize the reduced part of the electrolyte at the counter electrode. The ef®ciencies for conversion of solar to electrical energy can be quite high for high-quality single-crystal or thin-®lm semiconductor electrodes. However, in general these devices are very expensive to construct. Polycrystalline semiconductor electrodes, on the other hand, are much less expensive but usually their ef®ciencies are determined by processes occurring at grain boundaries (such as recombination of photoexcited electrons with positive holes) rather than by inherent characteristics of the semiconductor materials. A major problem with solar photoelectrochemical cells is the corrosion and degradation of the semiconductor surface.25 It is possible to minimize this problem by using an n-type semiconductor electrode with suf®ciently high band gap (> 3 eV, such as TiO2 )26 to make it stable, but this has a negative result: namely, the photon energy must be so high to be absorbed that only a 25

A silicon electrode, for example, lasts only a matter of minutes in most aqueous electrolytes. Titanium dioxide (TiO2 ) exists in two crystalline forms with different band gaps: anatase (Eg ˆ 3:23 eV, corresponding to 384 nm); and rutile (Eg ˆ 3:02 eV, corresponding to 411 nm). It is quite stable in photoelectrochemical processes, but it does corrode slowly in 1 M acids such as H2 SO4 or HClO4. It is nontoxic and is one of the cheapest and most widely available metal oxides, currently being primarily used in house paints. 26

727

15. ENERGY

small fraction of the sun's spectrum can be utilized. One method of overcoming this disadvantage is by using a visible light-sensitive dye adsorbed to the high-band-gap stable electrode.27 This approach also allows the exciting photon to be photoabsorbed by the adsorbed dye molecule, not by the semiconductor, which means that a photogenerated positive hole is not produced, and therefore ef®ciency-reducing electron±hole recombination that takes place in solid-state photovoltaics cannot occur. 15.5.5.2 Direct Solar Energy Production of Chemical Fuels: Hydrogen

We shall show in Section 15.8.3.1 that electrolytic dissociation of water, producing molecular hydrogen and oxygen, is one of the most promising methods of chemical energy storage. Photoelectrolysis of water (i.e., direct solar-to-chemical energy conversion) can also be carried out in a non regenerative photoelectrochemical cell if the band gap of the photosemiconductor is at least 1.229 eV (1000 nm), which is the difference between the H2 O=H2 and H2 O=O2 electrode potentials.28 If the semiconductor electrode is an n-type (see Section 15.5.4), the valence band positive holes react with the water to produce O2 at the semiconductor surface, the overall electrode reaction in acidic solution being29 1 2h‡ ‡ H2 O ! O2 …g† ‡ 2H‡ 2

…15-8†

(h‡ is a positive hole) and electrons reduce H2 O at the counter electrode: 2e ‡ 2H‡ ! H2 …g†

…15-9†

On the other hand, with p-type semiconductor photocathode electrodes, the roles are reversed: the photoexcited electrons reduce water to H2 at the semiconductor surface and water is oxidized to O2 at the counter electrode by the positive holes.

27

B. O'Regan and M. GraÈtzel, Nature, 353, 737±740 (1991); M. K. Nazeeruddin, A. Kaye, I. Rodicio, R. Humphrey-Baker, E. MuÈller, P. Liska, N. Vlachopoulos, and M. GraÈtzel, J. Am. Chem. Soc., 115, 6382±6390 (1994); A. J. McEvoy and M. GraÈtzel, Solar Energy Mater. Solar Cells, 32, 221±227 (1994) and following papers in Issue No. 3; M. GraÈtzel, Renewable Energy, 5, 118±133 (1994); M. GraÈtzel, Prog. Photovoltaics, 8, 171±185 (2000). 28 This difference does not depend on whether the electrolyte is acidic or basic, although the individual standard electrode potentials do. Thus, at 298 K in acidic solution E8…H2 O=H2 † ˆ 0:0 and E8…H2 O=O2 † ˆ 1:229V, whereas in basic solution E8…H2 O=H2 † ˆ 0:828 V and E8…H2 O=O2 † ˆ 0:401 V. See Section 9.4. 29 Note that this is equivalent to 1 H2 O ! O2 …g† ‡ 2H‡ ‡ 2e 2

728

15.6 GEOTHERMAL ENERGY

The ®rst demonstration of this direct method of solar dissociation of water was carried out with an n-TiO2 semiconductor electrode.30 The ef®ciency of hydrogen production was low, however (1%), since as pointed out in Section 15.5.5.1, the energy gap of TiO2 is over 3.0 eV, resulting in very poor utilization of the total solar radiation reaching the earth's surface. The ef®ciency can be improved by using semiconductors for both electrodesÐan n type for one and a p type for the other. When both electrodes are simultaneously illuminated, the sum of the two energy gaps contributes to the energy needed in the dissociation. An example of such a two-semiconductor photoelectrode cell is one containing an n-GaAs electrode coated with manganese dioxide and a platinum-coated p-Si electrode. It is worth noting that the space-charge layer exists near the semiconductor± electrolyte interface even if the semiconductor is not part of an electrochemical cell (i.e., even if it is not connected to an inert counter electrode by an external circuit). Therefore, dissociation of water can occur simply on the surface of illuminated semiconductor particles suspended in the electrolyte. Advantages of this method include that the particles can have very high surface-to-volume ratios (if colloidal, e.g.), and that very expensive crystal growth or thin-®lm deposition processes are unnecessary. The obvious major disadvantage of this technique is that the products of water dissociation (hydrogen and oxygen) are both gases and therefore are evolved together, making it dif®cult to recover hydrogen as a fuel. On the other hand, if dissolved hydrogen sul®de, H2 S, rather than water is dissociated in a sul®de electrolyte, the oxidized product sulfur forms a variety of polysul®des in solution, the overall reaction being …n

1†H2 S…aq† ‡ S2 …aq† ! …n

1†H2 …g† ‡ S2n …aq†

…15-10†

Elemental sulfur can subsequently be separated from the sul®de solution as a solid. Hydrogen sul®de is an abundant by-product of crude oil desulfurization and low-purity natural gas. An appropriate semiconductor has been found to be platinum-catalyzed CdS; although this undergoes photoanodic degradation, it is stabilized in a high concentration of sul®de ions. The ef®ciencies of several of the foregoing photoelectrochemical cells for the production of hydrogen have been shown to be reasonable and have encouraged ongoing research and feasibility studies.31 However, to date there have been no studies carried out utilizing them in pilot-scale facilities. 15.6 GEOTHERMAL ENERGY Hot springs and geysers occur in many parts of the world and are visible evidence for the reserves of thermal energy present in the earth. Two applica30

A. Fujishima and K. Honda, Nature, 238, 37±38 (1972). J. R. Bolton, `Solar photoproduction of hydrogen: A review', Solar Energy, 57, 37±50 (1996).

31

15. ENERGY

729

tions of this geothermal energy are possible: local or district heating, as is widely practiced in Iceland and parts of France and Hungary, for example, and generation of electricity. Principal geothermal electric generation sites are more localized; they include California, Italy, New Zealand, and the Philippines. In 1997 twenty-seven countries were using over 11,000 MW of geothermal energy for various heating purposes, while twenty-one countries generated 7000 MW of electricity (over a third of it in California) from these sources. One estimate suggests that there is as much energy available in accessible thermal reservoirs worldwide as in all the coal deposits. Further development of such sources is technologically feasible, and in appropriate locations they may be expected to contribute signi®cantly to future energy supplies. The 2000 MWth Nesjavellir power plant in Iceland illustrates a dual use facility. Steam and water are taken from boreholes 1 to 2 km deep and are used in part to provide steam at 1908C and a pressure of 12 bar to generate 60 MWe of electricity, and in part to provide 1100 l=s water at 1008C for heating purposes in Reykjavik and surroundings (1999 values). This water is transported via an insulated pipeline 25 km long with a temperature drop of about 18C. Although steam and hot water issue naturally from geothermal sources, practical utilization of these involves drilling wells into the heated strata. Three types of system are possible. 1. Dry steam, that is, steam accompanied by very little water, is the simplest system and is produced by some reservoirs. The steam can be used directly to power turbines for the generation of electric power. 2. Wet steam, which is steam mixed with a considerable amount of hot liquid water, is the most common geothermal energy source. Indeed, the liquid usually predominates. These waters, which have been in contact with hot rock under pressure, contain large concentrations of dissolved minerals that give rise to severe problems of corrosion and scale deposition from precipitation of dissolved substances. Three approaches to the use of such energy sources are as follows: (a) Separation of the liquid from the steam, and use of only the latter for power generation (b) Use of turbines capable of operating with a two-phase mixture (c) Use of the mixture or the hot water to vaporize a second, low boiling liquid such as isobutane to operate a turbine in a so-called binary system (a closed cycle is required for the working ¯uid, which must be condensed and reused) 3. Hot, dry rock is a potential energy source, although thermal reserves of this sort are not in use at present. For use, holes would be drilled into the porous or fractured rock, water pumped into some of them, and steam collected from others.

730

15.7 WIND AND WATER

The environmental effects of geothermal power plants have been discussed for one particular example by Axtman.32 Many of the problems are expected to be common to geothermal sources in general. Most obvious is the hot water waste from condensed steam, geothermal water, and condensed cooling water, although some hot water would be released naturally, regardless of whether it is used, from most reservoirs. Since the temperature of geothermal water and steam is comparatively low (of the order of 100±4008C), the thermal ef®ciency of power generation from these sources is low in comparison to a modern fossil fuel plant, and a large fraction of the thermal energy of such a system is waste unless used for secondary heating. In addition to the thermal pollution problem, the high mineral content of geothermal waters can be highly corrosive to equipment and can be a hazard, particularly since signi®cant amounts of toxic materials such as arsenic and mercury may be present. This, of course, depends on the composition of the rocks at the source. Injection of waste geothermal waters back into the system could avoid the pollution problem and also prolong the useful life of the source. A second pollution potential arises from gases released with the steam and water. The CO2 released may exceed that from an equivalent fossil fuel plant, and hydrogen sul®de is a common constituent. Small amounts of many other gases may be released, depending on the source, but one of major concern is radioactive radon, which occurs in some geothermal sources. Although there are other possible problems, such as earth subsidence, for the most part the environmental problems associated with geothermal energy do not seem to be great.

15.7 WIND AND WATER 15.7.1 Introduction The winds and waters of the earth offer abundant renewable energy, if their energy can be harnessed economically. Since few, if any, chemical reactions are involved in its use, it is free of most of the chemical pollution problems associated with fossil, nuclear, and even geothermal sources.

15.7.2 Wind Energy Conversion Wind was one of mankind's earliest sources of energy. Windmills have been used to pump water and perform other kinds of mechanical work for centuries, 32

R. C. Axtman, `Environmental impact of a geothermal power plant,' Science, 187, 795 (1975).

731

15. ENERGY

but they have been used only since the latter part of the 1800s to produce electric power. After the oil shortages of the 1970s (Section 15.1) and the pressures for developing environmentally benign energy sources, however, major efforts were made to harness wind energy. The United States, through the use of incentives provided by the 1978 Public Utility Regulatory Policies Act, state and federal tax credits, and a guaranteed utility electricity market, has until recently been the leading country in the development of wind turbines and wind farms. The early 1980s expectations for utilization of wind power were overly optimistic, partly owing to poorly designed wind turbines, high capital costs of installation, and little `bene®t' to public utilities to improve the equipment. However, great advances in new turbine performance and reliability have been made, and it appears that there are now no technological barriers to signi®cantly greater usage of wind power. In fact, wind power is now the second fastest growing energy source in the world. In 2000 total global power capacity of wind turbines was approximately 17.3 GW, with roughly 15% of this in the United States, and the amount is growing about 22% per year. Almost all the existing wind farms in the United States are located in California in three major mountain passes. The wind farm at San Gorgonio Pass, between Los Angeles and Palm Springs, consists of 3500 turbines (Figure 15-14). But we see in Figure 15-15 that

FIGURE 15-14 A typical wind farm in California.

732

15.7 WIND AND WATER

20

150 100

100

50

200 200

150

0

0

>300

30

0 20 0 15

200 >400

400 300 400

50

>50

50

80%); their usable lifetimes are long, and in general they seldom experience power outages and maintenance shutdowns. They emit no atmospheric pollutants. Construction of dams to form storage reservoirs often leads to other advantageous uses such as ¯ood control, irrigation, and recreation, although the concomitant submergence of land areas may have adverse environmental, economical, and recreational effects, particularly in agricultural or wilderness areas. The damming of rivers can affect wildlife habitat, particularly where wetlands used by migratory birds and shallow pools needed for spawning of ®sh are submerged below layers of sand in deep water. Damming can also have a negative in¯uence on the migration of ®sh, although this can be substantially mitigated in some cases by installing appropriate ®sh ladders or elevators, and by controlling operations to allow young ®sh to bypass turbines. In a dramatic policy reversal, at the time of this writing the government is considering the removal of several small power dams in the eastern and western parts of the United States, particularly where the loss of power would be minimal compared to the impact the dams continue to have on migratory ®sh. The gradual deposition of silt (siltation) may affect the capacities of storage reservoirs behind dams. Generally this effect is negligible in forest-covered areas, but it may be enormous in regions such as desert areas that receive violent rainstorms and are not protected by vegetation or where there is concurrent deforestation of the watershed. 15.7.3.2 Tidal Power

Energy can be extracted from the rise and fall of ocean tidesÐan enormous source of power. Extraction of tidal power is quite simple in principle. A tidal dam or ``barrage'' across an estuary creates an enclosed basin for storage of water at high tide. Turbines in the barrage are used to convert the potential energy resulting from a difference in water level ultimately into electrical energy. There are ®ve ways that tidal barrages can operate to generate electricity. The simplest (and probably the most economical) is ebb generation, where

735

15. ENERGY

¯ow is toward the sea at low tide. Reverse ¯owÐfrom sea to basin at high tideÐis ¯ood generation. A modi®cation of ebb generation is ebb generation plus pumping: the turbines are operated in reverse soon after high tide to pump water into the basin (to give a net energy gain, the additional water is released at a higher head than when it was pumped). Here the advantage is that electrical generation can start sooner than with ebb generation alone. Twoway generation utilizes ¯ow in both directions. In the two-basin generation scheme, which provides smoother power output, two interconnected water reservoirs are used. There are several environmental concerns with tidal power. Obviously, construction of a tidal barrage across an estuary changes the natural scenery. It also affects water quality (salinity, turbidity, dissolved oxygen, bacteria, sediment), ®sh and ocean fowl, and surface travel, since strong currents are produced and tides are modi®ed within the estuary. The oldest large tidal power scheme operating in the world (commissioned in 1966) is the 320-MW barrage at La Rance, near Saint-Malo, France (site of a twelfth-century tidal mill), where the mean tidal range is about 8 m but is 13.5 m during the spring equinox. The other currently operating scheme is a 20-MW pilot program at Annapolis Royal in the Bay of Fundy, Nova Scotia, Canada, commissioned in 1985. (The Bay of Fundy has the largest listed mean tidal range in the world, 11.28 m.) It is now estimated that tides of at least 5 m are required for tidal power to be economically feasible in competition with other energy sources. In the United States, only the southern part of the Bay of Fundy (Passamaquoddy Bay), with a mean tidal range of about 5.4 m, meets this criterion. Work was started there on a 110-MW two-basin scheme in 1935 but was abandoned the following year when it was determined that normal hydroelectric sources in Maine were more economical. Other sites in the world at which extensive economic feasibility and engineering studies have been carried out over the past 20 years, include the Severn and Mersey estuaries on the west coast of England and Wales, and sites in Russia and China. Tidal power is a truly renewable and predictable energy source. Carefully designed and constructed tidal barrages, while requiring several years for construction, are expected to last many years. Unfortunately, the economics are such that electricity to be produced many years in the future has little present value. Its real value, though, may be very large when accessible oil reserves are depleted or when the discharge of atmospheric pollutants from combustion of fossil fuels becomes a major concern. 15.7.3.3 Wave Power

Wave energy comes from the winds as they blow across the oceans. As such, the wind energy is concentrated in the water near its surface and is attenuated only over large distances.

736

15.7 WIND AND WATER

The ®rst patent describing a wave energy device was issued about 1800 in France, and an apparatus constructed near Bordeaux, France, in 1910 used the oscillations of seawater in a vertical bore hole to pump air that ran a turbine, producing 1 kW of electrical power. Small wave power generators have been in use for over 25 years for navigational aids. However, much research and development has been undertaken, particularly since the energy crises of the 1970s, in several of the developed maritime countries. Viable commercial facilities are now actively being developed in Japan, Norway, and the United Kingdom. (It is estimated that if the entire coastlines of these three countries were to be used to convert wave to electrical energy, the percentages of the 1985 national electricity demand would have been 15, 50, and 15%, respectively; for the United States, it would have been 7%.) There are many ways to convert wave energy to more usable forms; as with other forms of renewable power, though, it is important that the systems be rugged and simple. The most practical method now appears to be the pneumatic technique. Basically this system, shown in Figure 15±16, consists of a capture chamber (in which wave energy is trapped), which produces an oscillating water column that pumps an air turbine mounted above the water surface. Generally the capture chamber is designed to resonate with the wave frequency, but chambers can also be constructed that have two resonance frequencies, one for the chamber and one for the column, which in effect

Generator Turbine Float

Center pipe capture chamber

Mooring chain

FIGURE 15-16 Wave energy conversion chamber. From M. E. McCormick and Y. C. Kim, eds., ``Utilization of Ocean WavesÐWave to Energy Conversion,'' American Society of Engineers, New York, (1987).

737

15. ENERGY

makes it possible to double the energy production. In practice, many air chambers that match the frequency of the incident wave are combined. Oscillating water column systems can be ¯oating, as on a ship, or shore-®xed. A 10year study using a ¯oating system known as the KAIME I was undertaken by Japan in 1976. This system generated approximately 620 kW of instantaneous maximum power and an annual energy output of 190 MWh. Norway has constructed a shore-®xed multiresonant prototype power station in the 500kW range on its west coast at Tofteshallen. Wave power stations attenuate wave motion and thus make waves less steep, which may tend somewhat to reduce beach erosion. The greatest environmental effect of wave energy converters probably will be on non-bottomfeeding ®sh. There is also the possibility of interference with shipping, ®shing, and ocean recreational activities. In general, though, environmental impact problems appear to be much less severe than those of virtually any other energy conversion process. The various renewable energy sources discussed in Sections 15.5±15-7 are summarized in Table 15-5. Many of the quantitative estimates given in that table may be expected to change with further technological development.

15.8 ENERGY STORAGE 15.8.1 Introduction If large thermal or nuclear power stations are operated below a fairly narrow range of their rated output capacity, fuel consumption does not decrease in proportion to the decrease in electricity output. This leads to a waste of fuel and increased unit power cost. On the other hand, power demand is not constant over the seasons or even over a single day, being the greatest usually in midmorning and evening and the lowest after midnight to early morning. Thus, appreciable savings are possible if such plants can be operated full time near maximum capacity, with the excess electricity stored during low-demand periods and released quickly during peak demands. Similarly, solar energy is intermittent. Direct usage during sunlight hours may be adequate in some applications, but it is obvious that for increasing long-term utilization of solar energy (as well as other ¯uctuating renewable energy sources such as wind power), some auxiliary storage is required to provide effective continuous energy supply. We have already seen in Section 15.5.3 that water (e.g., solar ponds), rocks, molten salts, and liquid sodium are frequently used for solar energy storage as sensible and=or latent heat. These are short-term and limited-capacity storage means, however, and generally not suf®cient for large-scale usage.

738

15.8 ENERGY STORAGE

TABLE 15-5 Comparison of Renewable Energy Sourcesa Energy source

Capital cost ($U.S.=kW)

Anticipated Delivered cost change in capital cost over next ($U.S.=kWh) decade

Advantages

Disadvantages

Water pollution; requires large land area (competes with food production); may lead to some biodiversity loss; energy input may be a large fraction of output

Biomass

2500±3500

30±50% decrease

0.05±0.08

CO2 emission-neutral; usable for base and peak energy loads; large potential

Solar thermal

2000±4000

25% decrease

0.10±0.25

Negligible environmental Considered to be a highpollution; potentially risk technology usable over  408 latitude; plant sizes from small (10 kW) to large (hundreds of megawatts); usable with other energy sources (hybrid)

OTEC 5000±25,000 (ocean thermal energy conversion)

25±35% decrease

0.06±0.32

Negligible environmental Probably will need to use pollution; desalinated by-products to be economically viable; water and mariculture desirable by-products very low ef®ciencies

Photovoltaic 8000±35,000

40±50% decrease

0.25±1.50

Negligible environmental Intermittent; very high pollution; modular; no capital and production moving parts; costs; large land areas eventually should have needed for big plants; low operating and very dependent on maintenance expenses location

0.015±0.05

Commercially feasible; capable of large-scale base load electrical power generation

0.04±0.10

No emissions; can range Intermittent; possible from few hundred impact on wildlife and watts to manybird migration; megawatt stand-alone undesirable visual and applications; already sound effects cost-effective in some applications

Geothermal  2000

Wind

800±3500

20±35% decrease

Noxious emissions (e.g., H2 S) and water pollution unless reinjected; available only in discrete locations

(continues)

739

15. ENERGY

TABLE 15-5 (continued) Energy source

Capital cost ($U.S.=kW)

Hydro

1000±2000

Tidal

 1500

Wave

1600±7000

Delivered Anticipated change in capital cost cost over next ($U.S.=kWh) decade Slight increase

0.01±0.03

Advantages

Disadvantages

May occupy large land Most developed form areas; disruption of of renewable energy; water ¯ow pattern provides electric may seriously impact generating and ``pumped storage'' the ecology downriver capabilities; automatic and in adjacent areas; self-replenishing; large affects ®sh migration dams can control ¯ooding and provide irrigation and recreation Very limited sites No emissions; available; may have predictable source of major impact on water energy; practical from quality, ®sh, and small to mega scale marine mammals; produces strong currents; modi®es tides; may lead to sediment buildup or erosion

0.04±0.33

Negligible environme ntal pollution; potential for decreasing beach erosion; possible simultaneous mechanical water desalination)

Minor effects on marine environment; variable with weather; low ef®ciency, available only near coast (potential for negative visual and ecological impact on coastal areas)

a

Cost estimates are those available in 1998 and are subject to change Sources: Key Issues in Developing Renewables. Report of the International Energy Agency, OECD, Paris, 1997. The Future for Renewable Energy: Prospects and Directions, EUREC Agency, James & James, London, 1996. N. Cole and P. J. Skerrett, Renewables Are Ready: People Creating Renewable Energy Solutions, Chelsea Green, White River Junction, VT, 1995. R. J. Seymour, ed., Ocean Energy Recovery: The State of the Art, American Society of Civil Engineers, New York, 1992. U.S. Department of Energy website: http//geothermal.id.doc.gov/

A key parameter for evaluating and comparing various means of storing energy, particularly for powering mobile vehicles where weight may be a controlling factor, is energy density (or, perhaps more correctly, speci®c energy).

740

15.8 ENERGY STORAGE

This is the energy stored in the carrier, in watt-hours or kilowatt-hours, per kilogram of material (Wh=kg or kWh=kg). For example, we have seen (Section 15.5.3.1) that calcium chloride hexahydrate can store 2:8  105 kJ=m3 ; this is equivalent to an energy density of 0.045 kWh=kg. A typical 12-V lead±acid storage battery (Section 15.8.3.2) has a useful energy density of about 0.03 kWh=kg. Advanced thermochemical heat storage technologies have energy densities as high as 1.1 kWh=kg.

15.8.2 Physical Energy Storage 15.8.2.1 Pumped Storage

Pumped storage is an extension of hydroelectric power. Electricity is in effect stored as potential energy by pumping water up to a high-level reservoir during off-peak load periods and released to a lower level (usually at least 100 m) through turbine power plants during peak power demands. This is an established ¯exible and proven technology. Maximum output can be attained in less than one minute, and the overall ef®ciency of such a pump-discharge cycle can be as high as 65±75%. In the United States alone, total pumped-storage electricity capacity in 1999 was approximately 19 GW. Instead of pumped water, compressed air can also be used for energy storage. Off-peak electricity is used to pump air into underground caverns, apparently at considerably less cost if the appropriate cavern (either natural or excavated from rock or salt) is already available. Electricity is generated by withdrawing air and heating and expanding it through gas turbines. This technique was pioneered by Germany with a 290-MW plant at Huntdorf, and in Alabama a 500,000-m3 salt dome reservoir now being used for stored pumped air is capable of generating 110 MW of electric power for 26 hours. 15.8.2.2 Flywheels

An electrically run spinning ¯ywheel stores energy by converting electrical energy into mechanical energy of rotation. Ideally, in the absence of a load, it runs freely without friction by rotating on noncontacting magnetic bearings in an evacuated chamber. (But even with bearings of this type, ¯ywheels will lose on the order of 0.1% of stored energy per hour.) In essence it acts both as a motor (the electric current spins the wheel) and as a generator (magnets mounted in the ¯ywheel produce an electric current). These devices are particularly attractive for storing solar energy because a direct-current motor can be used to power them and an alternating-current motor can be used to remove the stored energy; thus they can serve as a dc-ac converter. Although

741

15. ENERGY

they can be very ef®cient (> 70%) and may have an energy density as high as 0.15 kWh=kg, rotational velocities as high as 100,000±200,000 rpm may be necessary for practical applications, requiring high-strength composite material. To date a fully integrated ¯ywheel system (sometimes called an electromechanical ¯ywheel battery) has not been demonstrated, although such units are being developed for stationary energy storage (where large units can be buried for safety purposes in the event of a ¯ywheel ``explosion'') and for automotive propulsion. 15.8.2.3 Superconductivity

Superconductors have zero resistance, and therefore virtually no energy loss in the absence of an applied load. This means that a coil made out of a superconducting material can serve as an energy storage device: electric energy, fed into the coil, is conducted almost inde®nitely until it is withdrawn as needed. One problem, however, is that the known superconducting materials exhibit superconductivity only at low temperatures. The critical temperature Tc is the temperature at which the resistance suddenly drops to zero. Before 1986 the highest known Tc was about 23 K. Since then new materials, such as the nonstoichometric oxide of yttrium, barium, and copper, YBa2 Cu3 O7 x (where x  0:1), and mercury-based cuprates have led to Tc values well above the boiling point of nitrogen (77 K, ±1968C). This means that liquid nitrogen, which is plentiful and cheap, can be used as coolant instead of the much more expensive liquid helium. However, the new ``high-Tc '' superconducting materials are very expensive, and construction costs will undoubtedly be quite high. For example, the storage units probably will have to be underground to control twisting forces from the high electric currents in the coil and to allow for possible coolant failure and the resultant loss of superconductivity, which would lead to violent release of the stored electric energy. Other engineering and fabrication problems exist, but the technology looks promising, and several prototype systems are currently being developed.

15.8.3 Chemical Energy Storage 15.8.3.1 Hydrogen

Hydrogen can be produced from the dissociation of water (an inexhaustible source) by several means, and it can be stored and transported over long distances by well-established techniques. It has excellent combustion properties and can be used in virtually all applications now primarily fueled by fossil sources such as power stations, internal combustion engines, and many other household and industrial areas. Its stored chemical energy can be converted

742

15.8 ENERGY STORAGE

directly to electrical energy by a fuel cell.36 Based on energy utilization by combustion to water, it has an energy density of about 40 kWh=kg of hydrogen,37 and catalytic burning of H2 gives high heat value with an ef®ciency greater that 95%. It has, however, a wider ¯ammable range, lower ignition energy, and higher ¯ame velocity when mixed with air than do most gas and liquid hydrocarbon fuels, making it a more hazardous material than most fossil fuels. We saw in Section 15.5.5.2 that experimental techniques using photosensitive semiconductor electrodes are being developed for the photoelectrolysis of water by direct solar-to-chemical energy conversion. However, electrolysis of water has been commercially available for over 80 years. It is one of the simplest methods for producing hydrogen, and in fact is the only process virtually free of pollutants when carried out with electricity produced from renewable primary energy sources such as solar energy (i.e., solar to electrical to chemical energy). Electrolysis of water is up to 95% ef®cient and has the advantage that the H2 and O2 products are physically separated when produced.38 Conventionally the electrolysis is carried out ( 908C) at atmospheric pressure in aqueous 25±30% KOH solution with nickel-plated steel or steel gauze electrodes, with the electrodes separated by a thin membrane. Hydrogen is evolved at the cathode 2H2 O ‡ 2e ! 2OH ‡ H2 …g†

…15-11†

and oxygen at the anode 1 2OH ! H2 O ‡ O2 …g† ‡ 2e 2 with the sum of the two giving the net two-electron decomposition 1 H2 O ! H2 …g† ‡ O2 …g† 2

…15-12†

…15-13†

36 Fuel cells are electrochemical cells that convert chemical energy, in the form of a continuous supply of fuel, directly into electrical energy. See Section 15.9. 37 Chemicals generally have energy densities from 1 to 10 kWh=kg. Hydrogen is exceptionally large because of its low molecular weight. 38 It should be pointed out that at the present time electrolysis is too expensive (primarily because of the cost of electricity) to be used on a large scale for the production of hydrogen. Industrial hydrogen is almost exclusively produced by the catalytic steam reforming of hydrocarbons  m H2 Cn Hm ‡ nH2 O „ nCO ‡ n ‡ 2

and the water-shift reaction CO ‡ H2 O „ CO2 ‡ H2 However, this method involves a nonrenewable feed source (hydrocarbon), and therefore it is not functioning as an energy storage procedure. It also generates CO2 , a greenhouse gas (see Section 3.1.2).

743

15. ENERGY

The theoretical cell potential for the dissociation of water is 1.229 V at 258C and 1 bar; in practice, this is higher because of electrode surface overvoltages and resistive losses. (Most of the energy loss is at the oxygen electrode.) Processes are being developed to carry out the electrolysis of water at temperatures as high as 9008C. One of the major advantages of operating at a high temperature is that the electrical energy required is decreased with increasing temperature.39 However, there are yet-to-be-solved problems in adequate high-temperature materials and construction techniques. Water can be dissociated in combination (hybrid) thermochemical±electrochemical processes or by purely thermochemical means. As an example, the Mark processes involve as a ®rst step the endothermic high-temperature ( 10008C) dissociation of sulfuric acid: 1 heat H2 SO4 ƒƒƒƒ! H2 O ‡ SO2 ‡ O2 2

…15-14†

SO2 ‡ 2H2 O ! H2 SO4 ‡ 2H‡ ‡ 2e

…15-15†

The thermal energy can come from combustion, nuclear, or solar sources. In the hybrid process, this is followed by an electrochemical step in which the SO2 is oxidized back to H2 SO4 and hydrogen gas is evolved by the reduction of H‡ : 2H‡ ‡ 2e ! H2

…15-16†

SO2 ‡ 2H2 O ! H2 SO4 ‡ H2

…15-17†

giving the overall reaction

In the purely thermochemical process, the oxidation of SO2 and formation of H2 occurs in the presence of I2 catalyst via a complex cyclic process involving polyiodides and sulfuric acid intermediaries as well as other catalytic decomposition reactions. The advantage of the purely thermochemical method is that thermal energy is converted into chemical energy (the H2 and O2 products of the dissociation) without ®rst converting the heat into mechanical energy and then into electrical energy. Since, however, these are multistage processes with some stages that involve highly corrosive materials, equipment and apparatus costs become an important factor in comparing these techniques to conventional water electrolysis. Several demonstration pilot plants are currently in use. 39 This is shown as follows. The electrical energy required is equal to DG, the change in the Gibbs function. At a constant temperature T,
G ˆ
H TDS. For the dissociation of liquid water, both the change in enthalpy and the change in entropy are positive: DH ˆ 285:8 kJ=mol and DS ˆ 163:3 JK 1 mol 1 at 258C. Therefore, assuming DH and DS are independent of temperature (a reasonable ®rst approximation), DG decreases with increasing temperature.

744

15.8 ENERGY STORAGE

Hydrogen can be stored as a gas or as a liquid, or chemically, or cryoadsorbed (adsorption at low temperatures). It is the least expensive long-term energy storage medium among electrochemical systems. Because of its low volume density, however, gaseous hydrogen generally has to be compressed for feasible storage. The triple point of hydrogen (the temperature at which solid, liquid, and gas are in equilibrium) is 14 K, its normal boiling point is 20.4 K, and its critical temperature is 33.3 K. Although liquefying hydrogen at 20 K increases its density by a factor of 845, the costs of cooling and storage at this low temperature (e.g., about 30% of its combustion energy is required to cool and condense it) make liquid storage economically unrealistic for large-scale storage or transport over long distances. An example of solid chemical storage of hydrogen is the exothermic formation of regenerable metal hydrides M ‡ xH2 „ MH2x

…15-18†

where M can be a metal such as magnesium, titanium, zirconium, or lanthanum, or intermetallic compounds or mixtures of metals (alloys). Nickel and its alloys are particularly promising, and metals such as magnesium doped with 5±10 wt% nickel show greater storage capacity and better cycling (hydrogenation=dehydrogenation) stability than the metals alone. The theoretical maximum energy density of nickel-doped magnesium hydride as a hydrogen storage material is about 3 kWh=kg. Hydrogen can also be converted to other molecules such as ammonia or methanol for easier storage and transportation, but at the cost of energy for its subsequent release. It is also cryoadsorbed below 77 K (the boiling point of liquid nitrogen) on a variety of active surfaces of different materials, such as active carbon, which increases the energy density of the hydrogen. However, both metal hydrides and cryoadsorbed hydrogen materials are affected by repetitive cycling. Another technique being studied for hydrogen storage is the use of carbon nanotubes with diameters the size of several hydrogen molecules; tubes are bundled together and hydrogen is drawn into them, making essentially a lightweight hydrogen sponge. 15.8.3.2 Batteries

A battery is an electrochemical cell in which stored chemical energy is spontaneously converted to electrical energy. This produces an electric potential across the cell's two electrodes, which are separated in the cell by an electrolyte solution (or sometimes a solid ionic conductor), and generates a current through a connected external load. Electrochemical reactions occur at the electrodes: reduction, a gain of electrons, at the cathode; and oxidation, a loss of electrons, at the anode. Many commonly used consumer batteries are discarded when most of the chemical energy has been converted (the cell has

745

15. ENERGY

been discharged). For a battery to function as an intermediate energy storage device, however, it must also be capable of being rechargedÐthat is, of restoring its chemical energy from electrical energy, generated, for example, by photovoltaic solar cells. To be an effective storage battery a device also must be able to cycle through this charge=discharge process many times. The most commonly used rechargeable storage battery for photovoltaic solar energy storage and for mobile vehicles40 is the lead±acid battery, made up of one or more series-connected cells. Each cell in the charged state consists of a solid (sponge) lead (Pb) electrode, a solid lead dioxide (PbO2 ) electrode, and an aqueous sulfuric acid electrolyte. Upon spontaneous discharge, the Pb is oxidized to solid PbSO4 at the negative electrode, Pb…s† ‡ H2 SO4 …aq† ! PbSO4 …s† ‡ 2H‡ …aq† ‡ 2e

…15-19†

and the PbO2 is reduced to solid PbSO4 at the positive electrode: 2H‡ …aq† ‡ H2 SO4 …aq† ‡ PbO2 …s† ‡ 2e ! PbSO4 …s† ‡ 2H2 O…l†

…15-20†

with the net cell discharging reaction being Pb…s† ‡ PbO2 ‡ 2H2 SO4 …aq† ! 2PbSO4 …s† ‡ 2H2 O…l†

…15-21†

The reverse reactions occur on charging. Maintenance-free, hermetically sealed lead±acid units are now being produced. A major disadvantage of these for applications requiring portability, however, is their relatively low energy storage capacity of 0.03 kWh=kg (see Section 15.8.1). They also have a limited cycle life, they contain toxic and environmentally damaging materials, and they are damaged by complete discharge and overcharging (deep cycling), which removes active solid material from the electrodes, as well as by high operating temperatures. Environmental contamination from lead in manufacturing and in disposal or recycling processes is also of concern (see Section 10.6.10). The nickel±cadmium (NiCd) battery is also used commercially in solar cell storage applications and in some experimental electric vehicles. When charged it consists of a cadmium negative electrode, a positive electrode of nickel oxohydroxide NiOOH
H2 O (with some graphite for conduction), and an aqueous potassium hydroxide electrolyte. When being discharged, cadmium is oxidized to Cd…OH†2 Cd…s† ‡ 2OH …aq† ! Cd…OH†2 …s† ‡ 2e

…15-22†

and the oxohydroxide is reduced to Ni…OH†2 2NiOOH
H2 O…s† ‡ 2e ! 2Ni…OH†2 …s† ‡ 2OH 40

…15-23†

At the time of this writing, commercially available electric vehicles require roughly 1 kWh to travel 10 km.

746

15.8 ENERGY STORAGE

giving the net spontaneous cell reaction Cd…s† ‡ 2NiOOH
H2 O…s† ! Cd…OH†2 …s† ‡ 2Ni…OH†2 …s†

…15-24†

Initially NiCd batteries are more expensive than the comparable lead±acid systems and have only slightly higher energy density (0.05 kWh=kg). However, they can tolerate more extreme operating temperatures and greater cycling depthsÐfor example, they can be completely discharged and=or overcharged without permanent harmÐhence generally have a longer design life ( 20 years). They also can be hermetically sealed. Since the hydroxide ion is neither a reactant nor a product in the overall reaction, the density of the electrolyte solution, potassium hydroxide, does not change during charging or discharging, in contrast to the lead±acid battery. However, cadmium is a toxic, environmentally undesirable material (Section 10.6.7), and proposals have been made in the European Union to phase out (ban) the use of these batteries. The battery that appears at this time to be the most probable replacement for the lead±acid battery in future electric vehicles is the rechargeable nickel± metal hydride (NiMH) battery.41 We have seen that hydrogen can be stored in a solid metal hydride phase (Section 15.8.3.1). In the nickel±metal hydride battery, the negative electrode is an appropriate metal hydride, MH,42 and the positive electrode is solid nickel oxohydroxide (as in the NiCd battery), with a concentrated KOH aqueous electrolyte. Upon discharging (the reverse reactions occur during charge), the hydrogen in MH is oxidized to water, MH ‡ OH ! M ‡ H2 O ‡ e

…15-25†

and nickel oxohydroxide is reduced to nickel hydroxide [reaction (15-23) ], giving the overall discharge reaction NiOOH
H2 O ‡ MH ! Ni…OH†2 ‡ M ‡ H2 O

…15-26†

This battery has a nominal voltage of 1.2 V and an acceptable energy density of approximately 0.07 kWh=kg. It can be sealed, and it has an appreciably longer lifetime than a comparable lead±acid battery. However, the nickel metal hydrides are very expensive to prepare and in the long run may be environmentally unacceptable. Another system that may turn out to have a reasonable energy density is the lithium ion cell. (The name comes from the exchange of lithium ions between 41

S. R. Ovshinsky, M. A. Fetcenko, and J. Ross, A nickel metal hydride battery for electric vehicles, Science, 260, 176±181 (1993). It is worth noting that a NiMH battery is now being used in the hybrid Toyota Prius automobile. 42 M is usually a metal alloy, optimized to give the most desirable physical and chemical properties. A conventional alloy for metal hydride batteries is LaNi5 mixed with rare earth elements such as Ce, La, Nd, and Pr. The proprietary MH electrode of the Ovonic battery (Ovonic Battery Co., a subsidiary of Energy Conversion Devices, Inc.) consists typically of a V, Ti, Zr, Ni, and Cr alloy.

747

15. ENERGY

the positive and negative electrodes during charging and discharging.) Electrochemical cells using lithium electrodes can theoretically produce a higher voltage than lead±acid or NiCd cells, and this in principle can lead to lighter weight storage batteries and therefore higher energy densities (0.15 kWh=kg). However, lithium metal reacts violently with water, forming LiOH and H2 . This means either that a nonaqueous electrolyte solution (such as lithium ion salts dissolved in organic compounds) must be used or that the lithium atoms need to be ``inactivated''Ðfor example, by intercalating43 them in an appropriate solid that binds them so tightly that they do not react with water. An example of the former is the Li MnO2 battery, in which Li is the negative electrode, solid MnO2 is the positive electrode, and the electrolyte is lithium perchlorate (LiClO4 ) dissolved in a mixed organic solvent such as propylene carbonate and 1,2-dimethoxyethane. The spontaneous discharging reactions are Li ! Li‡ ‡ e

…15-27†

MnIV O2 ‡ Li‡ ‡ e ! MnIII …Li‡ †O2

…15-28†

and

with the overall net reaction Li ‡ MnIV O2 ! MnIII …Li‡ †O2

…15-29†

One advantage of using cells of the latter type (where the lithium atoms are ``inactivated'') is that a relatively cheap aqueous electrolyte can be used. A promising experimental rechargeable cell has been developed44 with an aqueous 5M LiOH electrolyte that utilizes solid intercalation compounds such as LiMn2 O4 and VO2 as the electrodes in the completely discharged cell. During the charging process, some lithium is oxidized and removed from LiMn2 O4 at the positive electrode xLiMn2 O4 ! xLi…1

1=x† Mn2 O4

‡ Li‡ ‡ e

…15-30†

and the lithium ion is reduced and intercalated into vanadium oxide at the negative electrode, yVO2 ‡ Li‡ ‡ e ! yLi…1=y† VO2

…15-31†

so that the overall charging reaction is xLiMn2 O4 ‡ yVO2 ! xLi…1

43

1=x† Mn2 O4

‡ yLi…1=y† VO2

…15-32†

Intercalation is the reversible insertion of a substance into the bulk of a solid material. W. Li, J. R. Dahn, and D. S. Wainwright, ``Rechargeable lithium batteries with aqueous electrolytes,'' Science, 264, 1115±1118 (1994). 44

748

15.8 ENERGY STORAGE

Thus, the spontaneous discharge of the cell, which is the reverse of reaction (15-32), represents the removal of intercalated lithium from Li…1=y† VO2 and its intercalation into Li…1 1=x† Mn2 O4 . This cell has a working voltage of about 1.5 V, and it is estimated that a practical battery constructed of these materials would have an energy density of the order of 0.055 kWh=kg. However, safety is a major problem in scaling up to the battery sizes that would be necessary for economic use in electric vehicles. Another rechargeable lithium ion battery is the lithium polymer system, in which the problem of reaction between lithium and the solvent is eliminated by using a polymer matrix membrane, such as lithium perchlorate in polyethylene oxide, to separate the negative lithium metal electrode from the positive electrode. The negative electrode is made of polymer-bonded graphite attached to metal foil; passive ®lms that form on the surface prevent reaction with the electrolyte (a solution of lithium hexa¯uorophosphate in propylene carbonate and other solvents), yet allow relatively free passage of Li‡ ions during current ¯ow. The positive electrodes are made from metal (nickel, manganese, or vanadium) oxides. The sodium±sulfur battery has two molten electrodes (a molten sodium anode and a molten mixture of sulfur and sodium polysul®des cathode) with a solid b- aluminaÐnominally Na2 O
11Al2 O3 Ðelectrolyte that allows transport of sodium ions at elevated temperatures. When discharging, sodium is oxidized at the negative electrode Na…l† ! Na‡ …solv† ‡ e

…15-33†

and sulfur is reduced to polysul®des at the positive electrode: 2Na‡ …solv† ‡ xS…solv† ‡ 2e ! Na2 Sx …solv†

…15-34†

where x ˆ 3±5. The net cell reaction is 2Na…l† ‡ xS…solv† ! Na2 Sx …solv†

…15-35†

Sodium and sulfur are cheap and readily available. They are light elements and have a large reaction energy (the battery has a theoretical energy density of about 0.15 kWh=kg, more than four times that of the lead±acid battery, and an energy ef®ciency of approximately 85%), so it can be light and compactÐan important property for propulsion of electric vehicles. The major disadvantage is that the battery must be operated between 300 and 3508C to keep the sodium, sulfur, and polysul®des lique®ed, as necessary to obtain suf®cient electrolyte conductivity.45 These liquids can be very corrosive and hazardous. The zinc±air battery also has a high energy density (0.15±0.2 kWh=kg), and the materials used in its construction are relatively cheap compared with most of the other batteries that have been described. The oxidizing agent (oxygen) 45 b-Alumina is still a solid at these temperatures, but even as a solid it is as conductive at 3008C as is the liquid sulfuric acid electrolyte in the lead±acid battery at room temperature.

749

15. ENERGY

comes from the surrounding air rather than from material that is part of the battery, and this characteristic is largely responsible for the high energy density. During spontaneous discharge, zinc is oxidized at the negative electrode in a highly alkaline electrolyte to the zincate ion, Zn ‡ 4OH ! ‰Zn…OH†4 Š

2

‡ 2e

…15-36†

and oxygen from atmospheric air is reduced at a catalyst-activated carbon electrode, represented by the net reaction O2 ‡ 2H2 O ‡ 4e ! 4OH

…15-37†

to give the overall reaction 2Zn ‡ 4OH ‡ O2 ‡ 2H2 O ! 2‰Zn…OH†4 Š

2

…15-38†

In contrast to the electrical recharging already described for other rechargeable battery systems, the zinc±air battery being developed for possible large-scale utility energy storage and electric vehicle uses is recharged by recovering the spent zinc from the electrolyte and the metallic zinc electrode is mechanically replaced. Although we have focused attention on heavy-duty applications such as electric vehicles or power storage, many of these batteries already see much use on a much smaller scale in portable electronic devices and other consumer goods. A great deal of work is under way to improve performance in this area.46 Nonrechargeable batteries also see widespread use for these applications. They are also chemical energy storage devices in which energy is used to produce the reactive chemicals that go into them; but because the discharge reactions are not easily reversed, the batteries are used once and then discarded. (If recharging is possible at all with these types, it is usually to a small degree.) The most familiar nonrechargeable battery is the zinc±carbon dry cell, which consists of a carbon cathode (the positive pole), an aqueous paste of MnO2 and NH4 Cl, and an anode of zinc (which also acts as the container). The active elements are the zinc and MnO2 , which react to give zinc ions (as an ammonia complex) and MnO(OH). In practice, other additives may be present to enhance performance; in some designs these have included small amounts of mercury compounds. The alkaline manganese cell is similar, but the cathode is a compressed MnO2 ±graphite mixture, and the anode a powdered zinc±KOH paste; an absorbent material impregnated with KOH solution is the electrolyte. The reaction produces ZnO and Mn2 O3 . The mercury battery is another type of dry cell that was used extensively in cameras, medical equipment, and other devices requiring a more constant potential than is provided by conventional 46

M. Jacoby, Chem. Engi. News, 76 (31), 37 (1998).

750

15.9 DIRECT GENERATION OF ELECTRICITY FROM FUELS

dry cells. It consists of a zinc anode and a HgO±graphite (for conductivity) cathode and a concentrated KOH electrolyte. The cell reaction produces ZnO and Hg. Because of the hazard associated with mercury disposal, this type of cell is being phased out.

15.9 DIRECT GENERATION OF ELECTRICITY FROM FUELS All important electrical power generation from fossil fuels (and also from nuclear fuels) takes place by allowing the heat from burning fuel to vaporize a liquid, which in turn drives a mechanical device such as a turbine to operate a generator. The heat is rejected at some lower temperature determined by the water used for cooling the working ¯uid. The Carnot cycle ef®ciency limitations discussed earlier (Section 15.2.1) and other losses result in the waste of much of the energy of the fuel. A number of direct heat-to-electricity conversion processes have been proposed to eliminate the inef®ciencies associated with the mechanical steps, but they do not affect the heat cycle losses. Three methods of converting heat directly to electricity are the thermoelectric, thermionic, and magnetohydrodynamic conversions. Thermoelectric conversion operates on the familiar principle of the thermocouple: if two different conductors are made to form two junctions that are maintained at different temperatures, a potential difference and a ¯ow of electricity is set up between them. The thermionic process involves the emission of electrons from a heated cathode. These electrons are collected by an anode at lower temperature, and electricity can ¯ow in the external circuit between the two. In a magnetohydrodynamic generator, the fuel is used to heat and ionize a gas to produce a plasma. Passage of the plasma through a magnetic ®eld generates an electrical potential and current at right angles to the ¯ow of plasma. None of these has yet proven practical for commerical power generation use, although thermoelectric power units utilizing the heat from the decay of radioactive nuclei (e.g., 238 Pu) have been used for some time in special-purpose applications such as spacecraft. Direct conversion of chemical to electrical energy would also eliminate the Carnot cycle restriction, and may be done in fuel cells. A hydrogen fuel cell, for example, would involve the reaction47 2H2 ! 4H‡ ‡ 4e

…15-39†

at one electrode, and the reaction 47

As we have noted elsewhere (footnote 28), redox reactions involving hydrogen, oxygen, and water can be written with H‡ and H2 O or H2 O and OH depending on pH, but these are equivalent versions of the same reaction. Standard potentials are different but are related through the ion product of water (Chapter 9, Section 9.4).

751

15. ENERGY

:2 ‡ 4H‡ ‡ 4e ! 2H2 O

…15-40†

at the other. The overall reaction is the combination of hydrogen with oxygen to produce water, but if the two processes of reactions (15-39) and (15-40) take place at the surfaces of separate electrodes connected by an external conductor, the ¯ow of electrons necessary for the reactions can be used to do work. This work is equal to that required to transport the required number of electrons through the potential difference E of the cell. On a molar basis, this work is nFE, where n is the number of the electrons transferred in the reaction [4 in reaction (15-40)], and F is the value of the Faraday constant. If the process is carried out reversibly, the total energy available is equal to the free energy change of the process, that is, nFE

DG ˆ

…15-41†

Under these conditions, all the chemical energy is available to do work, and the theoretical ef®ciency is 100%. To obtain energy at a practical rate from an electrochemical cell, the cell would not in fact operate at equilibrium, and some energy would be lost. The actual potential V would be smaller than E, and the voltage ef®ciency can be expressed as ev ˆ

V E

…15-42†

Because a working cell would not operate under equilibrium conditions, it is more realistic to base an ef®ciency comparison on the enthalpy change of the reaction than on free energy. In this case the maximum intrinsic ef®ciency of an electrochemical energy-producing process is eˆ

DG DH

…15-43†

In most cases of interest, the calculated ef®ciency from equation (15-43) is greater than 80% (e.g., it is 83% for the H2 O2 cell). Some reactions have apparent ef®ciencies greater than 100% when calculated in this way; this happens if the entropy change is positive, making jDGj > jDHj. Such a cell must convert heat energy into power and would cool unless heat were provided to it from the surroundings. In this case both the energy of the fuel and the additional heat energy provided to the cell are converted to electricity. The foregoing theoretical ef®ciency does not allow for the losses in a real operating cell. The actual fuel ef®ciency of most fuel cells in practice is more typically in the 30±50% range, depending on the type; one must allow for energy that must be expended to supply the fuel, cool the system, and provide the required oxidant ¯ow, all of which may be signi®cant in a large cell. Nevertheless, ef®ciencies can be far greater than in a mechanical generator.

752

15.9 DIRECT GENERATION OF ELECTRICITY FROM FUELS

The cell electrodes must be separated by an ionic conductor (electrolyte) to permit transport of the hydrogen ions. This must be of low resistance to minimize internal voltage drop and heating, while preventing H2 and O2 from coming into direct contact with each other. Operating fuel cells generally employ hydrogen as the electroactive fuel, although this often is produced through reaction of coal, hydrocarbons or alcohols and the overall products in these cases are H2 O and CO2 . For largescale, economical operation, hydrogen derived from coal or natural gas is likely to be the preferred choice in the near future. In any event, a fuel processing unit is a necessary component in fuel cell power generation (although the solid oxide cell may be able to use natural gas without a reformer), and at the time of writing, a system for on-board conversion of gasoline to hydrogen for use in automotive fuel cells is in the development stage. Direct use of organic fuels, particularly methanol, has been studied extensively and would provide the most ef®cient operation, but such cells are not yet practical. However, studies are continuing. In any event, CO2 is a product unless H2 can be generated by nuclear, solar, or other non±fossil fuel means. Air is the most economical source of oxygen for these cells. Small amounts of NOx are also produced, but much less than from a traditional combustion source. Much research has been carried out on fuel cells over the past quartercentury to overcome the limitation of the small currents that can be transferred per unit area by most electrode materials. In many cases, expensive electrocatalytic materials such as platinum have been employed to obtain satisfactory high current densities at normal operating temperatures, although modern designs can use very small amounts or other, less expensive metals. Hightemperature cells avoid this problem, but materials become more expensive and corrosion becomes a major problem. The major cell types currently considered for large-scale use,48 categorized by electrolyte material (Figure 15-17), are as follows. 1. Alkaline cells, with an aqueous KOH electrolyte and using puri®ed hydrogen and oxygen. These cells have been widely used in the space program and are most developed. They are not expected to be economically suitable for electric utility generation, however. 2. Phosphoric acid cells, with hydrogen produced by steam re-forming of hydrocarbons or alcohols. These are being used in commercially available power generators with capacities of several megawatts.

48

J. Haggin, (Chem. Eng. News, p. 29, Aug. 7, 1995) summarizes demonstration applications of fuel cells for electric power generation as of mid-1995.

753

15. ENERGY

Anode

Electrolyte

Cathode

Anode exhaust,

Cathode exhaust

H2O (CO2)

H2O

Alkaline, 80⬚C H2 + 2OH–

H2O + 2e−

Platinum on graphite

Aqueous NaOH OH−

H2 H 2O Phosphoric acid, 200⬚C H2

+

2H +

2e−

Platinum on graphite

O2 Phosphoric acid H+

H2

+

2H + 2e−

H2

Molten carbonate, 650⬚C H2 +

2− CO3

CO2 + H2O +

2e−

Solid oxide, 1000⬚C 2−

H2 + O

Platinum on graphite

H2O + 2e−

Nickel H2 H2O CO2 Ceramic H2 H2O

H+- conductive polymer membrane H+ Molten Li2CO3 - Na2CO3 CO32− Zirconium oxide 2−

l/2O2 + H2O + 2e−

2OH−

l/2O2 + 2H+ + 2e–

H2O

l/2O2 + 2H+ + 2e−

H2O

l/2O2 + CO2 + 2e−

CO23−

Platinum on graphite O2 H 2O

H2 Polymer membrane, 80⬚C

Platinum on graphite

Platinum on graphite O2 H2O Nickel O2 CO2 Ceramic O2

l/2O2 + 2e−

O2−

O

Oxidant, O2 or air (CO2)

Fuel, H2

Direct

Current

FIGURE 15-17 Schematic illustration of the different types of fuel cells. (CO2 added to the cathode of the carbonate fuel cell may be recycled from the anode.) Exhaust will contain any unreacted fuel or oxidant. Cathode and anode half reactions are given.

3. Molten carbonate cells, using a molten alkali carbonate electrolyte at about 6508C. These have low internal losses, and at the time of this writing megawatt-sized plants are planned. High-temperature cells such as these are less dependent on high-purity reactants than the lower temperature types. 4. Solid oxide electrolytes at high temperatures give cells with high ef®ciencies, and several test units for power generation have been demonstrated. Natural gas may be used directly as the fuel. 5. Solid polymer electrolyte (proton exchange membrane) cells, which can produce high power densities because of their light weight, are beginning

754

15.10 THE ENERGY FUTURE

to be used in transportation and other applications requiring portability. Stationary power generation units are under test. High-temperature cells (i.e., the carbonate and solid oxide types) have practical ef®ciencies in the 50±60% range. They also produce waste heat at high temperatures that can be used in a steam cogeneration system. Phosphoric acid cells, which operate in the 40±45% ef®ciency range, with waste heat produced at low temperatures, are less attractive for supplemental energy generation use. Fuel cells have been used in specialized applications such as space vehicles since the 1960s and in demonstration power generation applications since 1992. Large-scale applications in electric utilities and in transportation are expected as further development brings costs down.

15.10 THE ENERGY FUTURE Any discussion of the energy future for either the United States alone or for the whole world is very dif®cult because of assumptions that must be made about population growth, industrial growth, changes in transportation, and political changes. Unforeseen political changes may occur at any time. For example, the political and economic collapse of the Soviet Union was not widely predicted before it happened, neither was the present trend to minimize emission of sulfur dioxide and greenhouse gases, if possible, in the developed countries. Nevertheless, a few comments will be made here.

15.10.1 The United States of America Before looking at the future, let us take a brief look at the past half-century. Energy production in the United States from 1949 through 1999 is shown in Figure 15-18. Because Figure 15-18 does not include imports, it shows considerably less petroleum and lique®ed natural gas products than we actually use. A complete energy ¯ow diagram that includes imports and exports for the United States in 1999 is shown in Figure 15-19. Both ®gures use the same unit of energy, the quad; Q1Q ˆ 1015 Btu ˆ 1:054  1018 J. Figure 15-20 shows the total energy consumption, the energy consumption per capita, and the energy consumption per 1996 dollar of gross domestic product in the United States from 1949 through 1999. Total energy consumption increased by about a factor of 3 in that time period, while per capita energy consumption increased by less than a factor of 2, and energy consumption per dollar of gross domestic product actually decreased. The U.S. population was about 150 million in 1949, increasing to 273 million in 1999. That

755

15. ENERGY

25 Natural gas 20

Quadrillion Btu

Crude oil 15 Coal 10

5 Hydroelectric power

Nuclear electric power Wood and waste NGPL

0

1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 Year FIGURE 15-18 Energy production by major source in the United States, 1949±1999. NGPL refers to natural gas plant liquids. From the U.S. Department of Energy, Information Administration website, http://www.eia.doe.gov.

the population increased much faster than the per-capita energy consumption and the energy consumption per 1996 dollar of gross domestic product actually decreased may be attributed to the energy conservation that followed the 1973±74 interruption of petroleum exports from the oil-producing countries in the Middle East and the concomitant rise in oil prices; this is sometimes referred to as the ``energy crisis'' or ``oil shock'' of 1973 and 1974. Figure 15-20 shows that nevertheless, this ``energy crisis'' resulted in only a short-term decrease in total and per-capita energy consumption in the United States. The post1973 low point in energy use occurred in 1983 after a period of high oil prices. Energy demand forecasts for the United States have been made by the Of®ce of Integrated Analysis and Forecasting, Energy Information Administration, U.S. Department of Energy, using the National Energy Modeling System (NEMS) up to 2020, a long time before nonrenewable resources like oil, natural gas, and coal run out. (It is very dif®cult to predict how long these nonrenewable resources will last because new reserves are still being discovered.) The modelers feel that the economy and the nature of energy

756

15.10 THE ENERGY FUTURE

Exports 3.82

Coal 1.53 Coal 23.33

Other 2.29

Natural gas 19.29 Cru de 12.5 oil 4

Fossil fuels Domestic 57.67 production 72.52

Supply 100.42

NGPL 2.51 Nuclear 7.73

Natural gas 22.10

Fossil fuels 81.56

Petroleum 37.71

Renewables 7.18

il s e o ct ud odu r C pr 53 . d an 22

Residential and commercial 34.17

Coal 21.70

Imports 26.92

Nuclear 7.73 Renewables 7.37

Consumption 96.60

Industrial 36.50

Transportation 25.92

Adjustments 0.98

Other 4.39

FIGURE 15-19 The energy ¯ow pattern in the United States in 1999. Units are quads (Q), and NGPL refers to natural gas plant liquids. From the U.S. Department of Energy, Information Administration Website, http://www.eia.doe.gov.

markets are reasonably well understood in this ``middle term'' time horizon. Figure 15-21 shows these forecasts of the energy use per capita and per dollar of gross domestic product (GDP) up to 2020 using real data through 1999. The projected future decrease in energy use per dollar of GDP, which follows the real decrease already mentioned, is partly the result of the Energy Policy Act of 1992 and the National Appliance Energy Conservation Act of 1987, which mandated energy ef®ciency standards for new energy-using equipment in residential and commercial buildings and for motors in industry. With the information available up to 1999, the projected energy use per capita was expected to increase slightly up to the year 2020.

15.10.2 The Rest of the World Prediction of global energy trends is much more dif®cult than forecasting for the United States, but, again, projections have also been made up to 2020 in the International Energy Outlook 2000 (IEO2000) from the U.S. Department of Energy. Figure 15-22 plots the known world energy consumption from

757

15. ENERGY

Energy consumption, 1949–1999 Quadrillion Btu

100 75 50 25 0

1950 1955 1960 1965 1970 1975 1980 1985 1990 1995

Energy consumption per person, 1949–1999

Million Btu

400 300 200 100 0

1950 1955 1960 1965 1970 1975 1980 1985 1990 1995

Thousand Btu per chained (1996) dollar

Energy consumption per dollar of gross domestic product, 1949–1999 25 20 15 10 5 0

1950 1955 1960 1965 1970 1975 1980 1985 1990 1995 Note: There is a discontinuity in this time series between 1988 and 1989 due to the expanded coverage of renewable energy beginning in 1989.

FIGURE 15-20 Total energy consumption, energy consumption per person, and energy consumption per dollar of gross domestic product in the United States, 1949±1999. From the U.S. Department of Energy, Information Administration website, http://www.eia.doe.gov.

1970 through 1997 and the projected world energy consumption through the year 2020, using three different predictions for world economic growth. In the case considered to be most likely at present, called the Reference case in Figure 15-22, the world is expected to consume 608 Q in 2020, an increase of 228 Q over 1995, with 66% of the increase attributed to the developing world, especially Asia and Central and South America (see Figure 15-23). The world gross domestic product (WGDP) grew by 4.3 trillion (1997 U.S. dollars) between 1970 and 1997 and is expected to almost double between 1997 and

758

15.10 THE ENERGY FUTURE

1.2 Energy use per capita

1.0 0.8 0.6 0.4

Energy use per dollar of GDP

0.2 History

0

1970

1980

Projections

1990

2000

2010

2020

FIGURE 15-21 Energy use per capita and per dollar of gross domestic product, 1970±2020 (index, 1970 ˆ 1). From the U.S. Department of Energy, Information Administration Website, http://www.eia.doe.gov.

800 High economic growth

Quadrillion Btu

600 Reference

400 Low economic growth

200

History

0

1970

1980

Projections 1990

2000

2010

2020

Year

FIGURE 15-22 World energy consumption by economic growth case, 1970±2020. From the U.S. Department of Energy, Information Administration website. Historical data from Energy Information Administration (EIA), Of®ce of Energy Markets and End Use, International Statistics Database and International Energy Annual 1997, DOE/EIA-0219(97), Washington, DC, April 1999. Projections from E=A, World Energy Projection System, 2000. Website, http://www.eia. doe.gov.

759

15. ENERGY

300 History

Projections

Quadrillion Btu

250 Industrialized

200 150

Developing 100 EE/FSU

50

0

1970

1980

1990

2000

2010

2020

Year

FIGURE 15-23 World energy consumption by region, 1970±2020. EE=FSU stands for eastern Europe=Former Soviet Union. From the U.S. Department of Energy, Information Administration Historical data from Energy Information Administration (EIA), Of®ce of Energy Markets and End Use, International Statistics Database and International Energy Annual 1997, DOE=EIA0219(97), Washington, DC, April 1999. Projections from EIA, World Energy Projection System, 2000. Website, http://www.eia.doe.gov.

2020, reaching 54 trillion by 2020. The IEO2000 projection makes many assumptions about oil prices and economic development in many parts of the world that may or may not be borne out. It is predicted that the ``energy intensity,'' usually shown in thousands of Btu per dollar of WGDP, will decrease in all parts of the world (see Figure 15-24). As one may imagine, energy forecasts change every year. As this volume is being written, they can be accessed on the World-Wide Web, starting with the U.S. Department of Energy, Energy Information Administration home page (http:==www.eia.doe.gov). World energy use forecasts, which give very similar results, are also made at intervals by the International Energy Agency (IEA) home page (http: ==www.iea.org). Other world energy forecasts, also giving similar results, are made by Petroleum Economics Limited (PEL), and Petroleum Industry Research Associates (PIRA). Figures 15-22 and 15-23 both show that the total energy used over the whole world is expected to increase in the future. The projections shown in these ®gures assume that the energy will come from fossil fuels, mostly because these projections were made with no regard for the Kyoto Protocol of December 1997, which could forestall much of the growth in energy

760

15.10 THE ENERGY FUTURE

Thousand Btu per 1997 dollar of GDP

60

History

Projections

50 40 30

EE/FSU

20 Developing 10 Industrialized 0

1970

1980

1990

2000

2010

2020

Year

FIGURE 15-24 World energy intensity (energy consumption per 1997 dollar of gross domestic product) by region, 1970±2020. EE=FSU stands for eastern Europe=former Soviet Union. From the U.S. Department of Energy, Information Administration. Historical data from Energy Information Administration (EIA), Of®ce of Energy Markets and End Use, International Statistics Database and International Energy Annual 1997, DOE=EIA-0219(97), Washington, DC, April 1999. Projections from EIA World Energy Projection System, 2000. Website at http://www.eia.doe.gov.

demand from industrialized countries.49 If the CO2 emission targets written into the protocol were to be achieved by reducing the use of fossil fuels, energy consumption would have to be reduced by 40±60 Q, about 10% of the total expected for the year 2020. Replacement of fossil fuels by biomass would recycle rather than increase CO2 emission, but the agricultural capabilities of the earth as a whole seem unlikely to be able to support the large-scale biomass program that would be necessary to make a major contribution while still producing food. Nuclear energy is the one obvious energy source that could substitute for fossil fuels without contributing CO2 to the atmosphere, but with the signi®cant problem of disposing of the accompanying radioactive waste. Large-scale nuclear power plants in some of the less stable underdeveloped countries are a disconcerting idea, since some of these facilities could be used to make nuclear weapons. Large hydroelectric potential is still available in some parts of the world, but only at the expense of major alterations in river

49

As of January 2000, the date used for the energy use projections, too few countries had rati®ed the Kyoto Protocol to make it effective.

761

15. ENERGY

¯ow and enormous dislocation of human beings; the Three Gorges project in China50 is an example. Economics is a limiting factor in any case, since most new energy sources are more expensive than fossil fuels. The ``bottom line'' in the energy future is that we really do not know what that future will be, but, if it is simply an extrapolation of the past, the consequences could be severe.

15.10.3 Conclusions It is virtually certain that energy use worldwide will increase because of increasing populations and continued development efforts in the presently underdeveloped nations. Continued reliance on fossil fuels causes problems quite apart from continued availability; these include possible effects on climate due to further increases of atmospheric carbon dioxide. Stabilizing CO2 emissions at somewhere near present values, or decreasing them, will be dif®cult to achieve as developing nations attempt to advance their economies. Although improvements can be made through conservation and increased ef®ciency, other energy sources seem essential. Many other energy sources yielding no or little pollution, as discussed in this chapter, can play a role, but most are limited with respect to location or amount. Table 15-5 summarized the current status of renewable energy sources. Cost is a critical factor. As long as fossil fuels remain inexpensive, other energy sources such as solar power, hydrogen fuels, and biomass will be unable to compete unless subsidized or their use mandated by regulation. In any event, costs will go up. Nuclear energy is the one tested source that has the potential for replacing carbon dioxide producing fossil fuels, but it has its own set of problems. These include waste disposal and the potential for radiation release, possible use of nuclear material by terrorist groups, and the risks of putting nuclear reactors in the hands of unstable or irrational governments whose leaders might divert nuclear fuels into weapons. In the United States, public fears of reactors and radiation are so strong that it is dif®cult to foresee much development in this ®eld. Even if built, reactors would be of high cost because of safety and licensing requirements. Other parts of the world have a different view. France, for example, generates most of its electricity from nuclear energy. Controlled nuclear fusion, highly touted as a future energy source, is too uncertain to be included in serious projections.

50 This project, to be completed in 2009, is forcing the resettlement of about 1.2 million people. The dam, across the Yangtze River, will be a 1.2-mile-long stretch of concrete with a reservoir about 400 miles long behind it.

762

ADDITIONAL READING

Additional Reading 15.1 Introduction Berger, J. J., Charging Ahead: The Business of Renewable Energy and What It Means for America. Henry Holt., New York, 1997. Schipper, L., and S. Meyers, Energy Ef®ciency and Human Activity: Past Trends, Future Prospects. Cambridge University Press, Cambridge, U.K., 1992.

15.3 Fossil Fuels Starr, C., M. F. Searl, and S. Alpert, Energy resources: A realistic outlook, Science, 256, 981 (1992). Preventing the next oil crunch. A series of articles by several authors. Sci. Am., pp. 75±95, March 1998. U.S. Geological Survey Circular 1118, 1995 National Assessment of United States Oil and Gas Resources. U.S. Geological Survey, U.S. Crude Oil, Natural Gas and Natural Gas Liquids Reserves, 1998, Annual Report. For a discussion of this report, see R. A. Kerr, USCS optimistic on world oil prospects, Science 289, 237 (July 14, 2000).

15.4 Nuclear Ahearne, J. F., The future of nuclear power, Am. Sci. 81, 24 (1993). Bodansky, D., Nuclear Energy, Principles, Practice and Prospects. American Institute of Physics Press, New York, 1996. Committee on Future Nuclear Power Development, Energy Engineering Board, Commission on Engineering and Technical Systems, National Research Council, Nuclear Power: Technical and Institutional Options for the Future. National Academy Press, Washington, DC, 1992. Darmstadter, J., and R. W. Fri, Interconnections between energy and the environment: Global challenges, Annu. Rev. Energy Environ., 17, 45 (1992). Levine, M. D., F. Liu, and J. E. Sinton, China's energy system: Historical evolution, current issues, and prospects, Annu. Rev. Energy Environ., 17, 405 (1992). Pace University Center for Environmental Legal Studies, Environmental Costs of Electricity. Oceana Publications, 1990. Rhodes, R., Nuclear Renewal: Common Sense about Energy. Viking Penguin, New York, 1993. Worledge, D. H., Role of human performance in energy systems management, Annu. Rev. Energy Environ., 17, 285 (1992).

15.5 Solar Energy 15.5.1 Introduction Scheer, H., The economy of solar energy, in Advances in Solar Energy, Vol. 9, K. W. BoÈer, ed., pp 307±337. American Solar Energy Society, Boulder, CO, 1994. Wieder, S., An Introduction to Solar Energy for Scientists and Engineers. Krieger, Malabar, FL, 1992. Zweibel, K., Harnessing Solar Power. Plenum Press, New York, 1990.

763

15. ENERGY

15.5.2 Biological Utilization of Solar Energy: Biomass Abrol, Y. P., P. Mohanty, and Govindjee, eds., Photosynthesis: Photoreactions to Plant Productivity. Kluwer Academic Publishers, Dordrecht, 1993. Bain, R. L., and R. P. Overend, Biomass electric technologies: Status and future development, in Advances in Solar Energy, Vol. 7, K. W. BoÈer, ed., pp. 449±494. American Solar Energy Society, Boulder, CO, 1992. Beadle, C. L., S. P. Long, S. K. Imbamba, D. O. Hall, and R. J. Olembo, Photosynthesis in Relation to Plant Production in Terrestrial Environments. Tycooly, Oxford, U.K., 1985. Biofuels. Energy and Environment Policy Analysis Series, International Energy Agency, Paris, 1994. Klass, D. L., Biomass for Renewable Energy, Fuel and Chemicals. Academic Press, San Diego, CA, 1998. Patterson, W., Power from Plants. The Global Implications of New Technologies for Electricity from Biomass. Earthscan Publications, London, 1994.

15.5.3 Physical Utilization of Solar Energy Avery, W. H., and C. Wu, Renewable Energy from the Ocean. A Guide to OTEC. Oxford University Press, New York, 1994. Cavrot, D. E., Economics of ocean thermal energy conversion, Renewable Energy, 3, 891±896 (1993). DeMeo, E. A., and P. Steitz, The U.S. electric utility industry's activities in solar and wind energy: Survey and perspective, in Advances in Solar Energy, Vol. 6, K. W. BoÈer, ed., pp 1±218. Plenum Press, New York, 1990. Hurdes, J. V., and B. Lachal, Industrial Solar Heat. Delta Energy, Schaffhausen, Switzerland, 1986. Kreider, J. F., and F. Kreith, Solar Heating and Cooling: Active and Passive Design, 2nd ed. McGraw-Hill, New York, 1982. LoÈf, G., ed., Active Solar Systems. MIT Press, Cambridge, MA, 1993. Nielsen, C. E., Salinity-gradient solar ponds, in Advances in Solar Energy, Vol. 4, K. W. BoÈer, ed., pp. 445±498. Plenum Press, New York, 1988. Takahashi, P. K., and A. Trenka, Ocean thermal energy conversion: Its promise as a total resource system, Energy, 17, 657±668 (1992).

15.5.4 Photovoltaic Utilization of Solar Energy Coutts, T. J., and J. D. Meakin, Current Topics in Photovoltaics. Academic Press, London, 1985. Fahrenbruch, A. L., and Bube, R. H., Fundamentals of Solar Cells. Photovoltaic Solar Energy Conversion. Academic Press, New York, 1983. Foraser, D. A., The Physics of Semiconductor Devices, 4th ed. Clarendon Press, Oxford, U.K., 1986. Fuhs, W., and R. Klenk, Thin-®lm solar cells, in Advances in Solar Energy, Vol. 13, D. Y. Gosami and K. W. BoÈer, eds., pp. 409±443. American Solar Energy Society, Boulder, CO, 1999. Green, M. A., Solar Cells: Operating Principles, Technology, and System Applications. PrenticeHall, Englewood Cliffs, NJ, 1982. Holl, R. J., and E. A. DeMeo, The status of solar thermal electric technology, in Advances in Solar Energy, Vol. 6, K. W. BoÈer, ed., pp. 219±394. Plenum Press, New York, 1990. Lasnier, F., and T. G. Ang, Photovoltaic Engineering Handbook. Hilger, Bristol, U.K., 1990. Maycock, P. D., and E. N. Stirewalt, A Guide to the Photovoltaic Revolution. Rodale Press, Emmaus, PA, 1985. MoÈller, H. J., Semiconductors for Solar Cells. Artech House, Boston, 1993. Neville, R. C., Solar Energy Conversion: The Solar Cell. Elsevier, Amsterdam, 1978. Treble, F. C., ed., Generating Electricity from the Sun. Pergamon Press, Oxford, U.K., 1991.

764

ADDITIONAL READING

15.5.5 Photoelectrochemical Utilization of Solar Energy Aruchamy, A., ed., Photoelectrochemistry and Photovoltaics of Layered Semiconductors, Vol. 14 of Physics and Chemistry of Materials with Low-Dimensional Structures, F. Levy, editor-inchief. Kluwer Academic Publishers, Dordrecht, 1992. GraÈtzel, M., ed., Energy Resources through Photochemistry and Catalysis. Academic Press, New York, 1983. Koval, C. A., and J. N. Howard, Electron transfer at semiconductor electrode±liquid electrolyte interfaces, Chem. Rev., 92, 411±433 (1992). McEvoy, A. J., and M. GraÈtzel, Sensitization in photochemistry and photovoltaics, Solar Energy Mater, Solar Cells, 32, 221±227 (1994). Memming, R., Photoelectrochemical utilization of solar energy, in Photochemistry and Photophysics, Vol. II, J. F. Rabek, ed., pp. 143±189. CRC Press, Boca Raton, FL, 1990. Norris, J. R., Jr., and D. Meisel, ed., Photochemical energy conversion, in Proceedings of the Seventh International Conference on Photochemical Conversion and Storage of Solar Energy, July 31±August 5, 1988. Elsevier, New York, 1989. Santhanam, K. S. V., and M. Sharon, eds., Photoelectrochemical Solar Cells. Elsevier, New York, 1988.

15.7 Wind and Water Asmus, P., Reaping the Wind, Island Press, Washington, D.C., 2001. Baker, A. C., Tidal Power. Peter Peregrinus, London, 1991. Dodge, D. M., and R. W. Thresher, Wind technology today, in Advances in Solar Energy, Vol. 5, K. W. BoÈer, ed., pp. 306±359. Plenum Press, New York, 1989. Jog, M. G., Hydro-Electric and Pumped Storage Plants. Wiley, New York, 1989. McCormick, M. E., and Y. C. Kim, eds., Utilization of Ocean WavesÐWave to Energy Conversion. American Society of Engineers, New York, 1987. Quarton, D. C., and V. C. Fenton, eds., Wind Energy Conversion 1991. Mechanical Engineering Publications, London, 1991. Raabe, J., Hydro Power. VDI-Verlag, DuÈsseldorf, 1985. Sesto, E., and C. Casale, Wind power systems for power utility grid connection, in Advances in Solar Energy, Vol. 9, K. W. BoÈer, ed., pp. 71±159. American Solar Energy Society, Boulder, CO, 1994. Shaw, R., Wave Energy. A Design Challenge. Ellis Howood, Chichester, U.K., 1982.

15.8 Energy Storage Bockris, J. O'M., B. Dandapani, and J. C. Wass, A solar hydrogen energy system, in Advances in Solar Energy, Vol. 5, K. W. BoÈer, ed., pp. 171±305. Plenum Press, New York, 1989. Bockris, J. O'M., and T. N. Veziroglu, with D. Smith, Solar Hydrogen EnergyÐThe Power to Save the Earth. MacDonald Optima, London, 1991. Bolton, J. R., Solar photoproduction of hydrogen: A review, Solar Energy, 57, 37±50 (1996). Chaurey, A., and S. Deambi, Battery storage for PV power systems: An overview, Renewable Energy, 2, 227±235 (1992). Douglas, T. H., ed., Pumped Storage. Thomas Telford, London, 1990. Gretz, J., Solar hydrogen, Renewable Energy, 1, 413±417 (1991). Mantell, C. L., Batteries and Energy Systems, 2nd ed., McGraw-Hill, New York, 1983. Pichat, P., Photochemical Conversion and Storage of Solar Energy. Kluwer Academic Publishers, Dordrecht, 1991.

765

15. ENERGY

Serpone, N., D. Lawless, and R. Terzian, Solar fuels: Status and perspectives, Solar Energy, 49, 221±234 (1992). YuÈruÈm, Y., ed., Hydrogen Energy Systems. Kluwer Academic Publishers, Dordrecht, 1995.

15.9 Fuel Cells Blomen, L. J. M. J., and N. M. Mugerwa, eds., Fuel Cell Systems. Plenum Press, New York, 1993.

15.10 Resources Starr, C., M. F. Searl, and S. Alpert, Energy resources: A realistic outlook, Science, 256, 981±987 (1992). U.S. Geological Survey Circular 1118, 1995 National Assessment of United States Oil and Gas Resources.

EXERCISES 15.1. Coal is combusted at 15008C to obtain the maximum amount of heat (Section 15.3.3). One ton (2000 lb) of bituminous coal (DHcombustion ˆ 35 kJ=g) is combusted in a Carnot cycle heat engine operating at maximum thermodynamic ef®ciency, with the excess heat discharged to a water reservoir at 688F (208C). The speci®c heat and density of water are 1.0 cal=g and 1:0 g=cm3 , respectively. Calculate the following: (a) The maximum thermodynamic ef®ciency of this engine (b) The amount of heat discharged to the river, assuming that the temperature of the river is unchanged (c) The amount of water in the reservoir if the amount of heat calculated in part b actually causes the temperature to rise to 718F. 15.2. The potential supply of hydrocarbons in tar sands and oil shale is said to be equal to all the crude oil reserves in the world. List the economic and environmental reasons why neither of these sources is used as a source of oil at the present time. When do authorities predict they will be used? Why? 15.3. (a) List the environmental problems resulting from the combustion of coal for the generation of electricity. Why is coal still being used on a large scale for the generation of electricity in the United States? (b) What are the economic and environmental advantages and disadvantages for the conversion of coal to methane (syngas). Why is this not done extensively today? Write the equation for the conversion of coal to methane. In writing your answer, remember that most coal contains the following elements: C, H, N, O, S.

766

EXERCISES

15.4.

15.5.

15.6.

15.7. 15.8.

15.9.

(c) Both nuclear and coal-®red power plants are used extensively for the generation of electricity. List the environmental advantages and disadvantages of each and then decide which is the more costeffective and the lesser source of environmental problems. Finally, assuming that you are the leader of the world, which would you decree should be used for power generation world wide. Explain your answer. A basic problem with the use of fossil fuels as an energy source is the emission into the atmosphere of the green-house gas carbon dioxide. Suggest how to burn carbon compounds without releasing carbon dioxide into the atmosphere (this is not discussed in this book). What are the environmental and economic costs of your solution(s) to the carbon dioxide emission problem? If you cannot come up with an idea to solve this problem look, for a possible solution in the scienti®c literature or on the World-Wide Web. Calculate the maximum (ideal thermodynamic) ef®ciency for (a) a PWR plant with steam to the turbine at 3308C and condenser temperature at 308C and (b) a coal-®red plant with steam at 5308C and the same condenser temperature. The net ef®ciencies are about 30 and 50%, respectively. Why are these less than the maximum? A certain nuclear power plant (an LWR with 3% enriched fuel) has a net electrical output of 1000 MWe and operates for 320 days per year. Assuming as an approximation that half the energy comes from the ®ssion of 235 U and the remainder from 239 Pu, how many kilograms of 235 U are ®ssioned? How many kilograms of ®ssion products are produced? How many gallons of fuel oil and how many tons of coal would be required to provide the same energy per year? Compare the relationship between energy utilization and the environment in the days of the Industrial Revolution and in the present. An electrical utility has asked for proposals to replace an aging 1000MWe nuclear power plant located in northeastern New York State. Presentations are to be made for replacing the NPP with (a) solar panels, (b) an array of windmills, and (c) a coal-®red plant. As a consultant, you have been asked to evaluate the three proposals. Select one of the options and prepare a statement containing the various reasons for and against selecting that option. Include a detailed statement on how the environment would be affected. As a variation, select a different U.S. location for the NPP that is to be replaced. In regions of the United States where deregulation of the electric utility industry has been partially or completely achieved, what consequences can be characterized as (a) ``expected'' and (b) ``unexpected''? How is deregulation affecting the environment?

15. ENERGY

767

15.10. How do you account for the fact that in different countries the attitude toward nuclear power ranges from strong opposition to indifference to opposition to the closing of an NPP? 15.11. Prepare an essay, a class presentation, or a term paper on one of the following. (a) The current status and future prospects for nuclear power in the United States, Europe, and Asia. This amounts to updating Tables 15-3 and 15-4 and adding comments. (b) The options available to the United States for decreasing the emission of greenhouse gases. Is lowering energy consumption a viable option? (c) Your personal attitude toward nuclear power and the basis for it. Discuss the extent that your attitude is in¯uenced by facts and by emotions. (d) What do you believe to be (not wish to be) the future of nuclear power in the United States? Why? How much of your belief is based on risk? On environmental impact? On political and other factors (to be identi®ed)? 15.12. Silicon is the most used semiconductor material for solar cells (Section 15.5.4). It has a band gap Eg ˆ 1:107 eV. (a) What is the wavelength, in nanometers of a photon of energy 1.107 eV? What spectral region is this? (b) Assuming a Boltzmann distribution of thermal energy [equation (42) ], calculate the fraction of Si atoms that possess an energy equal to 1.107 eV at 258C. 15.13. Make a list of the regions of the world that are most favorable for geothermal power generation. 15.14. What are the most likely environmental problems associated with geothermal power sources? 15.15. List the sources of renewable energy and summarize the advantages and disadvantages of each. In so far as you can, include economic considerations. 15.16. Write the electrode reactions that take place when an ordinary carbon± zinc dry cell is discharged. 15.17. When lead±acid batteries ``wear out,'' they must be disposed of or recycled. Describe the processes and hazards that would be involved in recycling them. Compare this to the hazards of disposal in a land®ll. 15.18. What are the electrode reactions (anodic and cathodic) in the various types of fuel cells? 15.19. Calculate the theoretical ef®ciency of a hydrogen±oxygen fuel cell operating at room temperature.

768

EXERCISES

15.20. What are the primary types of electric battery under consideration for electric power storage? For electric vehicle propulsion? Summarize the advantages and disadvantages in each case. 15.21. Search the Internet for the most recent predictions of energy use and compare them with those given in this chapter. If there are signi®cant changes, discuss the reasons for them.

16 SOLID WASTE DISPOSAL AND RECYCLING

16.1 INTRODUCTION Safe disposal of solid wastes is a serious problem. With our culture, which generates ever larger amounts of disposable materials and an increasing population density, we can no longer simply ``throw things away.'' If we discard them on land, they must be buried for aesthetic, safety, and health reasons. Even this is not enough, because toxic materials can be dissolved and enter the groundwater. Consequently, disposal site construction that minimizes leaching and includes elaborate leachate recovery systems is required; sites must be chosen carefully to ensure that the inevitable accidental breaches of the system used to seal the completed land®ll will have minimal impact. Remote sites increase transportation requirements, but of course, sites must not be in our backyards (NIMBY). Ocean disposal has potentially serious effects on ocean life and thus on a vital food supply, as well as having safety and aesthetic consequences when refuse materials wash up on beaches that are heavily used for recreation (see Chapter 1 for other comments on this). Some waste materials can be disposed of by burning. Unfortunately, combustion of many substances can generate toxic products that are released to the 769

770

16.1 INTRODUCTION

atmosphere and widely dispersed. Special incinerators and scrubbers may be necessary, and even these may not satisfy the concerns of those who live downwind. Recycling will reduce the amount of material to be disposed of. It has its own problems of collection, sorting, and cost. Composting of degradable organic materials also reduces disposal while producing a useful product, while anaerobic digestion is a possible source of methane fuel. A mix of these processes will be needed in future solid waste handling techniques. Municipal wastes, that is, those not including industrial wastes or hazardous materials, vary widely in composition. Sometimes they include demolition debris, industrial wastes, or water treatment sludge, for example. Most of the total municipal solid waste generated in the United States is disposed of in land®lls; according to 1998 EPA estimates, of the total 220 million tons of waste produced, 55% went to land®lls, 17% was incinerated, and 28% recycled. Waste generation is projected to continue to increase, while recycling is expected to take up a signi®cantly larger fraction. Disposal of hazardous wastes is a separate problem. Estimates of municipal waste production and recycling in the United States in 1998 are given in Tables 16-1 and 16-2 and recent trends are shown in Figures 16-1 and 16-2. TABLE 16±1 Waste Production and Recycling of Different Types of Material in the United States in 1998 Material

Weight generated (lb 106 )

Percent recycled

Paper=paperboard Plastics Glass Metals: Iron=steel Aluminum Other nonferrous Rubber and leather Textiles Wood Yard wastes Food wastes Miscellaneous materials Miscellaneous inorganic wastes

84.1 22.4 12.5

41.6 5.4 25.5

12.4 3.1 1.4 6.9 8.6 11.9 27.7 22.1 3.9 3.3

35.1 27.9 67.4 12.5 12.8 6.0 45.3 (composting) 2.6 23.1 Negligible

Source: EPA Environmental Fact Sheet: Municipal Solid Waste Generation, Recycling and Disposal in the United States: Facts and Figures for 1998. http://www.epa.gov/osw.

Container manufacturers Steel mills and detinning plants

Primary and secondary aluminum producers Plastic resin, ®lm, and ®ber manufacturers and processors

Glass

Tin cans

Aluminum cans

Plastic

Products of petroleum and natural gas distillation and re®nement

Re®ned bauxite, carbon

Iron ore, lime, coke

Sand, limestone, soda ash

Wood pulp, other plant libers

Virgin materials

>14,000

> 60

50±150

16

700

Number of manufacturers

30

8

80

11

85

Consumption (1989) (tons 106 )

Reduced energy consumption Cost savings Availability

Less costly feedstock Reduced water consumption Lower capital requirement Energy savings Cleaner furnace ®ring Potential furnace life extension Reduced capital requirements Reduced raw material requirements Higher quality input (if purchased from detinners) Avoided capital cost

Bene®ts

Source: L. F. Diaz, G. M. Savage, L. L. Eggerth and C. G. Golueke, Composting and Recycling Municiple Solid Waste, Lewis Publishers, Boca Raton, FL, 1993.

Paper and paperboard mills

Type of industry

Paper

Recycled material

Examples of Industries Using Recycled Materials as Feedstocks in 1989

TABLE 16-2

772

16.2 LANDFILLS

240

220

Millions of tons

200

180

160

140

120

100

80 1960

1970

1980 Year

1990

1998

FIGURE 16-1 Total municipal waste production in the United States. From data in EPA Environmental Fact Sheet: Municipal Solid Waste Generation, Recycling and Disposal in the United Stated: Facts and Figures for 1998. http://www.epa.gov/osw.

Containers and packaging, including cans and bottles, made up 72.4 million tons of waste in the United States in 1998, of which 40% overall was recycled; over half the steel and about 44% of the aluminum packaging (mostly cans) and over half the paper and paperboard packaging was recycled, but only 29% of the glass packaging materials. Nondurable goods provided 60.3 million tons of waste, with paper and paper products contributing 40 million tons in this category. Durable goods (appliances, etc.,) amounted to 34.4 million tons.

16.2 LANDFILLS Originally, land®lls were simply places where waste could be dumped where it did not disturb too many people. As problems associated with this form of

773

16. SOLID WASTE DISPOSAL AND RECYCLING

5

Pounds/person/day

4.5

4

3.5

3

2.5

1960

1970

1980 Year

1990

1998

FIGURE 16-2 Municipal waste production in the United States. From data in EPA Environmental Fact Sheet: Municipal Solid Waste Generation, Recycling and Disposal in the United Stated: Facts and Figures for 1998. http:==www.epa.gov=osw.

disposal became to be recognized, more elaborate arrangements became necessary. Many old land®lls that did not meet modern standards, or that were full, have been closed, and it is not a simple matter to open new ones. In the United States, operating land®lls went from about 8000 in 1988 to about 2300 in 1998. A modern land®ll is sealed underneath by a ¯exible membrane liner such as various forms of polyethylene, rubber, or poly(vinyl chloride) that resist degradation, and=or a layer of impermeable clay. Some of the properties of clays for this purpose were discussed in Section 12.3.1. A system for leachate collection also is necessary. The waste is placed in compacted, earth-covered layers, and, when the land®ll is full, closed by a water-impermeable top layer. Figure 16-3 is a schematic illustration of a land®ll with a double liner and double leachate collection system. Not all land®lls will have these redundant features.

774

16.2 LANDFILLS

Gas vent

Soil

Filter layer Waste

Low permeability clay

Flexible membrane liners

Porous layers

Leachate collection system

FIGURE 16-3 Schematic model of a modern land®ll.

The leachate collection system typically consists of plastic pipes leading to a sump with a pumping system to remove the liquid. The pipes are embedded in a porous layer that may be an appropriate soil or an arti®cial material. A ®lter layer screens out ®ne particles of earth that could clog the drainage system. Gases, chie¯y methane, are released as the organic materials in the waste decay. These gases must be controlled to avoid the buildup of potentially explosive concentrations. In some cases, the methane can be collected for use as a fuel. Although a typical land®ll is a pit, some are constructed as mounds above the surface. These above-grade deposits can be large (a popular name is Mount Trashmore); the largest is the Fresh Kills land®ll site on Staten Island, New York, which is expected to top out as a mound more than 150 m high, along with several smaller mounds, by 2005. This type of land®ll avoids excavation and makes leachate collection easier, but more earth must be brought into cover the trash layers, and the mound is more subject to erosion. When completed, the earth-covered mound can be used as a recreational area, as has been done at Virginia Beach and other locations, but any use must avoid penetration of the cap. Although biodegradable materials do decompose in land®lls, the process is not rapid. Conditions are anaerobic and not conducive to rapid biological action. Even after decades, newspapers have been recovered that are readable, and food items identi®able. In some sense, a land®ll can be regarded not as a disposal site but as a storage site.

16. SOLID WASTE DISPOSAL AND RECYCLING

775

On a volume basis, plastics are more important than their low weight percentage implies. They have low densities, often do not crush well, and have a tendency to work their way to the surface. Discarded automobile tires have a similar tendency, which is one reason many land®lls will not accept them. Although not nominally considered to contain hazardous materials, toxic substances from household chemicals, batteries, paint solvents, and so on inevitably make up some fraction of household wastes. However, EPA regulations prohibit disposal of hazardous wastes in an ordinary municipal land®ll. Hazardous wastes, which include ¯ammable, volatile, toxic, and pathological wastes, include wastes from many industrial operations. Radioactive wastes are a special class of hazardous material, discussed in Chapter 14. Hazardous wastes are often disposed of in land®ll facilities speci®cally intended for the purpose, and with extensive documentation. In the past, there was considerable mixing of hazardous and municipal waste and few records of land®ll composition or even location were kept; land®ll construction was much more casual. Accidental breaching of these disused land®lls has had serious effects, as illustrated by the notorious Love Canal1 site near Niagara Falls in New York State. Love Canal was a disposal site used by a number of ®rms for dumping of chemical wastes over a long period beginning in the 1930s. Sealed in the 1950s, the site was later used for school and housing development. Such use breached the clay cover that had sealed the site and allowed entry of water. Leaching of chemicals such as benzene and chlorinated hydrocarbons into basements and other sites of exposure caused considerable health risks requiring abandonment of the housing and the expenditure of millions of dollars in cleanup programs. This was the beginning of the program to identify potentially hazardous waste sites in the United States and the setup of the ``Superfund'' program to monitor them and clean them up. Many such sites exist. They are by no means con®ned to the United States; a situation very similar to Love Canal occurred in the Netherlands, where a new village (Lekkerkirk) was built on a waste dump in 1970 but had to be abandoned in the 1980s with large costs for cleanup. There are thousands of identi®ed abandoned and potentially hazardous waste sites worldwide, and probably many more that have not been identi®ed.

16.3 COMPOSTING Biodegradable organic materials have bene®cial effects when applied to agricultural land, in part as fertilizer because of their N, P, and K content (although this is typically relatively low), but mostly in terms of improving soil quality 1 Love Canal was an uncompleted navigation and electrical generation canal intended to bypass Niagara Falls. It was started in the late 1800s but abandoned with comparatively little excavated. The ``ditch'' left behind was later used as a site for waste disposal.

776

16.3 COMPOSTING

by increasing its organic content (see Section 12.3.1). Raw organic waste, such as food processing residues, garden wastes, or sewage sludge (if sterilized) can be applied directly, but composting provides important advantages. (The problem of heavy metal contamination of sewage sludge was referred to in Section 11.5.2; the same considerations apply if this sludge is used in composting.) Composting consists of breakdown of the organic material through microbial activity to derivatives of the lignins, proteins, and celluloses that resist further reaction. It produces a material with the characteristics of humus. Pathogens are destroyed during the process through the action of the heat that is generated. Temperatures of 55±608C for a day or two will kill most pathogens of concern, and such conditions are produced in normal composting behavior. Obviously, adequate mixing is essential, to avoid cold spots and to ensure that all pathogens spend adequate time in the heated regions. Composting of wastes that contain potentially large concentrations of human pathogens, (e.g., sewage sludge) must be done with careful control of conditions. Composting involves the interaction of the organic substrate with the organisms in the presence of water and oxygen to produce heat, carbon dioxide, and the decomposed organic materials. Conditions such as substrate composition, aeration, and moisture content affect the process and need to be well controlled to give a good quality product and to ensure operation of a large-scale plant. As with recycling, sorting is necessary to avoid contamination with nondegradable materials. Size reduction, particularly of waste wood, branches in yard waste, and so on, is necessary. The C=N ratio of the substrate strongly affects the rate, and nitrogen-rich materials may have to be added to act as fertilizer. The consistency of the material must allow air to circulate. Therefore the mix must have reasonable particle size and cannot be excessively wet. Materials such as sewage sludge need to be mixed with coarser materials, for example. The process is not rapid. Two weeks and usually more is required between the start of the process and its completion, so that a largescale composting plant will contain a large volume of material. One process is static; the organic waste is placed in an appropriate pile over a pipe that passes air into it, or applies suction to draw air through it. Odors can be trapped by a layer of ®nished compost, which has good adsorption properties. A second process involves the construction of windrows (elongated piles) of the waste, and mechanically turning and mixing them on a regular basis. These piles may be 6 or 7 ft high, 10 to 13 ft wide (narrower with manual turning), and as long as necessary. Shelter is needed for both these systems to keep out excessive moisture from rain, and for temperature protection in cold climates. Odor control is necessary for the windrow method. An alternate process, mechanical composting, involves the use of rotating drums, or tanks equipped with mixing devices along with aeration, to provide optimal aeration and mixing. These afford more rapid reactions in the initial steps of the process when the greatest generation of odor is likely, but still

16. SOLID WASTE DISPOSAL AND RECYCLING

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require considerable time either in the reactor or in a windrow stage for complete reaction to a usable material. Control of possible leachate from the wastes waiting to be processed, and from the composting materials, is necessary. As indicated, odor is one of the main concerns raised in objections to composting sites. Although the process is aerobic, some anaerobic decomposition can occur locally in the composting mass, generating typical anaerobic decay products such as ammonia, hydrogen sul®de, and organic sul®des such as mercaptans. Aerobic products such as low molecular weight fatty acids (e.g., acetic and butyric acids), aldehydes, ketones, esters, terpenes, and others with objectionable odors also may be released. A properly designed composting facility must have provision for capturing these materials, usually by passing the exhaust air through absorbers or scrubbers of some kind to either trap or chemically (sometimes biologically) destroy the obnoxious materials.

16.4 ANAEROBIC DIGESTION OF BIOLOGICAL WASTES It was pointed out in Section 11.5.2 that the volume of sewage sludge that must be disposed of can be minimized by anaerobic decomposition to produce methane, a useful by-product. This process can be extended to other organic waste materials, including animal and human wastes, domestic wastes and crop residues. The wastes are made into a slurry and digested by anaerobic bacteria over a period of weeks to produce a gas (called biogas) that is approximately 60% methane. Most of the remainder is carbon dioxide; undesirable components such as H2 S are usually quite low. The process can be quite simple and has applications as an energy source in undeveloped areas, since the biogas can be used for heating, cooking, or running engines. The digestion process uses a number of complementary bacterial species that convert protein, carbohydrate, and lipid material to simpler compoundsÐ amino acids, simple sugars, fatty acidsÐand ®nally into methane as the bacteria use these compounds to grow. Except for some chemicals that might be found in industrial wastes, composition of the waste is not critical. Operating conditions, such as temperature and pH, must be kept within certain limits for optimum gas production. The ®nal output from such digesters is a sludge containing half to two-thirds of the original organic content. This can be used as a fertilizer, although there may be concern about the complete destruction of pathogenic bacteria.

16.5 INCINERATION Combustible wastes have long been disposed of by burning. As is the case with burial, this solution is not simple when carried out on a large scale. Three

778

16.5 INCINERATION

major problems must be dealt with in burning of waste: smoke, soot, and ash released to the atmosphere; highly toxic compounds produced through incomplete combustion and also released to the atmosphere; and toxic residues, chie¯y heavy metals, that contaminate the ash and may enter groundwater from ash disposal. On the other hand, the volume of solid waste that must be disposed of in land®lls is markedly reduced, and the energy released in the combustion process may be recovered, either to produce steam for heating or to generate electricity. In all incineration processes, several possible modes exist for release of undesirable materials in the exhaust. These include material that escapes combustion (e.g., if the residence time is too short, or if the waste, is poorly mixed and does not experience suf®ciently high temperature), material that is only partially oxidized to other, perhaps more hazardous compounds, fragments from thermal decomposition (pyrolysis) of larger molecules (e.g., benzene rings, small chlorinated molecules), and new molecules that may form from partially decomposed material in temperature regions that are high enough to promote reaction but not high enough for decomposition to be complete. Dioxins are an example; their formation was discussed in Section 8.10.3. The presence of chlorine- or bromine-containing materials can lead to the formation of hazardous chlorinated or brominated organics, including halogenated dibenzofurans (Section 8.10.3) and biphenyls (Section 8.7), as well as HCl, while sulfur compounds will produce SO2 , and the combustion process itself will generate nitrogen oxides. Such incomplete combustion can release hydrocarbons, particularly polycyclic compounds such as benzo-(a)-pyrene,

as well as carbon monoxide. Other toxic elements present at trace concentrations in the waste, such as Se, As, and heavy metals, can also escape as ®ne particulates; ¯y ash is generally higher in heavy metal concentration than the coarse ash left in the incinerator, but even the latter may have enough heavy metal content to require special disposal. Various designs of incinerators are available for dealing with municipal wastes. They must allow thorough mixing of the waste with air and maintain a temperature high enough (750±10008C), along with a residence time of the combustible material in the hot zone long enough (at least 3±4 s) to permit complete degradation of all organic molecules to carbon dioxide. This may involve a two-stage combustion process. Exhaust gases must be scrubbed to remove HCl and other components, and particulate materials must be removed by electrostatic precipitators and ®lters.

16. SOLID WASTE DISPOSAL AND RECYCLING

779

For incineration of municipal waste, two approaches are in use. In mass burning, the waste is burned with only minimal preseparation (e.g., of oversize noncombustibles). Shredding or shearing of large combustibles is necessary to provide reasonable handling. Such incinerators may be used solely for waste disposal, or the heat generated may also be used as a source of energy. The heat value of municipal solid waste ranges from about 7,000±15,000 kJ=kg, depending on the composition (cf. anthracite coal, 30,000±37,000 kJ=kg). Plastic waste has the greatest heating value per unit weight, while paper and other combustble components are considerably lower. Combustion is a way of recovering some of the energy value of plastic and other wastes if recycling is not practical.2 Although incineration of large amounts of plastics generates more emissions of chlorine and of lead and cadmium from compounds that are still used as stabilizers, studies have shown that properly operating modern plants can maintain emissions well within safe limits. Complete combustion will preclude release of smoke containing soot, but ®ne ash particles and gaseous pollutants must be removed by precipitation and=or scrubbing of the stack gases as already mentioned. The waste normally contains considerable water, and under some conditions this will lead to a visible steam plume as the vapor condenses. A plume will form if, upon mixing of the warm stack gas with the ambient air, the temperature and relative humidity of the mix reach a value in which the saturation level of the air is exceeded. This is often interpreted by neighbors as harmful, although in itself it is not unless it hides particulate smoke. Ash, both the ®ne ¯y ash recovered from the gas stream and the coarser material left in the incinerator, must be disposed of, usually in land®lls. If the heavy metal content is low enough, however, the ash may be used as a ®ll or aggregate. Some material, especially ferrous metal, can be recovered from the coarse ash before disposal. If scrubbers are used to treat the stack gases, solid or sludge residues from these will also be placed in land®lls. While incineration as a municipal solid waste disposal method can be safe and effective, the technology is not easy to control because of the variable nature of the material to be burned. Even with careful selection, one can never be sure that a householder has not put some highly hazardous material into the garbage, and thus explosions when the waste enters the incinerator are possible. Care in maintaining the monitoring systems and in controlling the operating parameters is essential if release of highly hazardous organic byproducts is to be avoided. Municipal incinerators have been criticized not only because of their potential for release of materials to the atmosphere, but also because of their effect on recycling. The cost of construction, particularly if the facility is also used to generate energy, makes it necessary from an economic point of view to operate 2

B. Piasecki, D. Rainey and K. Fletcher, Am. Sci., 86, 364 (1998).

780

16.5 INCINERATION

an incinerator as continuously as possible. Consequently, removal of combustible materials from the waste stream for recycling may be discouraged. Also, ef®cient plants need to be large and consequently need large amounts of waste; transportation becomes a factor. The second approach to incineration of municipal waste is the use of refusederived fuels for energy generation. In this approach, the waste is ®rst processed for the recovery of recyclables and to assure a more uniform material that can be handled and burned in a more controlled fashion. The refusederived fuel is co-burned with another fuel, usually coal. Typically, in these coburning systems, 30% of the fuel, producing 15% of the energy, is refuse derived. This is the limit for regulations applying to coal-burning generators. If more refuse is used, more stringent rules requiring more monitoring of potential toxic releases go into effect. Various special purpose waste incinerators are in useÐfor example, to burn sewage sludge or hospital wastes. Hazardous wastes that are not highly combustible and must be burned at an appropriately high temperature for safety reasons are treated in incinerators with auxiliary gas or oil fueling. A large use of incineration is for the disposal of liquid industrial hazardous wastes. Wastes designated as hazardous may be disposed of in incinerators intended speci®cally for that purpose (e.g., Figure 16-4), but much is disposed of in industrial boilers or furnaces, such as the cement kilns discussed in Section 12.4.4. In fact, over half the hazardous wastes incineration in the United States is done in cement kilns. Incineration of hazardous wastes in the United States is governed by the fairly elaborate EPA Boilers and Industrial Furnace (BIF) regulations, which in summary call for minimum destruction of 99.99% (99.9999% for certain materials like dioxins) destruction of the waste. Notice that this is not a limit on the amount of unburned material that can be released in total, just a limit on the fraction of the input that can be released. There are other restrictions such as on CO, metal, and particle release. A well-designed combustion chamber can minimize stagnant regions that may not reach proper temperatures and maximize mixing, but operation under less than optimum conditions can defeat this. Because hazardous wastes are likely to be of variable composition (except for burners dedicated to incineration of a speci®c process stream), maintaining optimum conditions may not be easy. Monitoring release is also a problem because of the large number of possible products involved. Carbon monoxide monitoring can be used to indicate deviations from proper conditions but is not a direct measure of what is being released. Ocean incineration, carried out aboard special incinerator ships, has had some use. Here, the theory is that the incineration occurs far from any populated area, and any emissions will be absorbed by the ocean before they can be carried to land. This practice would permit incineration of very toxic materials,

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Chimney Storage tanks for liquid and pasty waste

Post combustion chamber Steamboiler

Electrostatic filter

Four-step gas washing

Feedhopper

Bunker for solid waste

Dediox filter

Rotary kiln incinerator Drum elevator Water purification

Drum storage

Incinerator ash

Boiler ash

Fly ash

FIGURE 16-4 Schematic of a rotary kiln hazardous waste incinerator. From http:==www.eurtits.org=reports=9702.htm. Used by permission of the European Union for Responsible Incineration and Treatment of Special Waste and Indaver.

but if carried out on a large scale raises questions about effects of toxic releases on the ocean food chain if combustion were not complete.

16.6 THE TIRE PROBLEM About 250 million worn-out automobile tires are discarded annually in the United States, and many more globally. Disposal of these waste tires has long been a problem. Land®lling is dif®cult because tires tend to work their way to the surface, as mentioned earlier. Open dumps, of which there are many, are breeding grounds for mosquitoes because of the stagnant water that readily collects in the tires, and they are subject to ®res that are both extremely smoky and notoriously dif®cult to put out. These ®res release toxic products and leave toxic residues. One tire ®re, in Winchester, Virginia, burned for nine months. A number of states have enacted legislation dealing with scrap tire disposal.

782

16.6 THE TIRE PROBLEM

However, nearly two-thirds of the tires now being discarded are not disposed of in any productive way.3 Useful rubber products are produced by vulcanization, a process that uses sulfur to cross-link the polymer chains of the raw rubber to give a material with physical and chemical properties that make it tough, stable, and nonbiodegradable. Fillers such as carbon black are added to improve properties, while tires also contain steel or ®ber reinforcing belts. Depolymerization of the rubber, while chemically feasible, is not economically practical. A number of processes can be used to pyrolyze the scrap tires to produce gaseous and liquid hydrocarbons useful as fuels or as chemical feedstocks, along with carbon black and recovered steel. Although these have promise, at the time of writing no commercial plants are operating, again because such enterprises are not economically viable. A couple of plants, one in Wind Gap, Pennsylvania, and another in Centralia, Washington, have operated intermittently, and a demonstration pilot plant has been built near Leipzig, Germany, in the town of Grimma. The major use of scrap tires at present is as tire-derived fuel. Whole or shredded tires, which have very high heat values, are used to supplement traditional fuels in cement kilns, pulp and paper mill boilers, and coal-®red power generating facilities. Growing use as fuel is anticipated as it becomes more commonly recognized that controlled combustion does not involve the smoke emissions associated with free burning. The properties of scrap tires make them directly useful for some purposes. They can be used to construct arti®cial reefs in which the tires are tied together and anchored in coastal waters, where they are attractive to barnacles and other marine organisms and for many types of ®sh. Tires can also be used to construct ¯oating breakwaters to protect harbors and beaches. Stacks of tires have been used as highway crash barriers at bridge piers and other obstructions and for the construction of retaining walls for steep-sided areas next to highways. In a number of states including Florida, West Virginia, Ohio, and Pennsylvania, scrap tires are used constructively in land®lls, either as a daily land®ll cover or as part of the leachate collection system. In some cases, the tires are shredded before use in land®lls. Shredded tires have many other applications. For example, the shreds have been used to make ¯oor mats and sandals and have been used as ®ll and insulation under road beds. Very small shreds, known as ground rubber, have been used for running tracks on athletic ®elds, railroad crossing beds, carpet underlay, and as an asphalt additive. In some cases, rubber strips cut from the tires are used to make dock bumpers, ¯oor mats, conveyor belts, and so on. In 1998, 23% of U.S. tires were recycled, excluding those used for fuel or recovered for retreading. 3

K. Reese, Today's Chem. Work, (#2), 75 (February 1995), provides a discussion of the 1994 situation.

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783

16.7 RECYCLING Recycling is an alternative to the waste disposal methods discussed in the preceding sections of this chapter. The present discussion will be mostly about ``municipal solid waste,'' which comes from households, commerce, industry, and government. The approximate composition of this municipal solid waste in 1998 and the percent of the different materials that were recycled were shown in Table 16-1. Some solid waste can be recycled in a variety of ways to make useful objects. Before any of the various materials that make up this solid waste can be recycled, however, they must be separated, at least in part. Separation at the point of origin provides cleaner, higher quality material than that separated from mixed solid waste, and many municipalities now encourage such separation, but even separated waste does not provide pure materials for recycling. Sometimes the separated but not pure solid wastes can be recycled as such, but often further separation is necessary. For example, as will be seen shortly, glass waste and beverage cans must be further separated before the materials can be reused. It is dif®cult to treat the economics and cost-effectiveness of recycling in isolation. In general, the improvement of the quality of the environment due to recycling has not been factored into the economics. In many cases, this makes many types of recycling appear to be cost-ineffective on purely economic grounds. In some cases, however, the use of recycled materials can be costeffective even without considering these intangible factors. Table 16-2 gave some examples of industries in the developed world that used recycled materials as feedstocks in 1989.

16.7.1 Glass The municipal solid waste stream contains about 10 wt % glass, most of which is container glass, the glass used to make jars and bottles: mayonnaise and pickle jars, beer bottles, wine and liquor bottles, some soft drink bottles, and so on. Container glass is the only glass that is being recycled in large quantities at present. Glass used in such items as light bulbs, drinking glasses, mirrors, and cookware is different in composition from container glass and is not accepted for recycling by the container industry. Glass pieces that can be recycled are called ``cullet'' and must often be color-sorted before reuse. Much cullet, called primary cullet, is generated during the manufacture of glass. Traditionally, about 15% of the material used in the manufacture of glass containers has been cullet, but a goal of 30±50% has been established within the container industry. It is actually advantageous to use cullet because it lique®es at a lower temperature than the raw materials: sand (SiO2 ), lime (CaO), and soda ash (Na2 CO3 ) used in the manufacture of glass. This results

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in energy savings (for every 1% of recycled glass used, there is a 0.5% drop in energy use) and the extension of the useful life of furnace linings, among other things. If the cullet is not color-separated, it is used for the production of glass beads, roadway materials, and building materials such as ®berglass insulation.

16.7.2 Paper Paper and paper products are made from wood and consist mostly of cellulose, as discussed in Section 7.3.2. Most paper products contain various additivesÐ ®llers such as clay or titanium dioxide, resins to improve wet strength, sizings, coloring, and so on. These differ depending on the type of paper, adding to the complications of paper recycling. Separation of paper to be recycled into various grades is required. As shown in Table 16-1, nearly 42% of the paper produced in the United States was recycled in 1998. The types of paper that are recycled are newsprint, corrugated cardboard, magazines, and so-called high-grade and mixed papers. Domestic demand for reclaimed papers has been rather erratic over the years, and a large amount has been exported: 6.5 million tons in 1990, for example, mostly to the Far East. In 1995, about 20% of all paper reclaimed in the United States was exported. Corrugated cardboard is the main reclaimed paper product that is exported. Recycled paper is used mainly by four different industries. The ®rst is the paper products industry, to make newsprint, various other writing and printing papers, bags, towels, and tissues. To use recycled newsprint for fresh newspapers, it must ®rst be de-inked in special de-inking mills that were in short supply until the mid-1990s. New de-inking plants were built only after a number of states required that a minimum percentage of recycled paper be used in newsprint. De-inking consists of repulping the paper in a solution of sodium hydroxide and hydrogen peroxide, along with surfactants to release the ink, which is separated by ¯otation. Other contaminants such as staples and glue must also be removed. The process breaks up the ®bers to some degree, reducing the quality of the product and limiting the number of times a given sample of paper can be recycled. To maintain quality, some percentage of virgin ®bers or higher quality paper (typically 30% coated paperÐmagazines, etc.) must be added to recycled newsprint. The second industry is the paperboard products industry, to make corrugated boxes, shoe boxes, and ®le folders. The third is the construction paper industry, to make roo®ng materials and acoustic tile. The fourth is the molded paper products industry, to make egg cartons and layers for packing fruit. Recycled paper products are also used to a small extent to make cellulose insulation, bedding for animals, mulch, and liquid and solid fuels.

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785

16.7.3 Metal The metal content of municipal solid waste consists mostly of aluminum or ferrous metals and these are generally recycled separately. 16.7.3.1 Aluminum

Aluminum scrap that is produced during the manufacture of aluminum products (new scrap) is almost completely reused and recycled. Old scrap comes from discarded aluminum products including cans, aluminum siding, lawn furniture, automobiles, pots and pans, and venetian blinds. Recycling of aluminum cans began in the early 1960s, encouraged by the major aluminum companies, and was viewed mostly in terms of public relations. By 1995, 65% of the aluminum from used beverage cans was recycled back to aluminum can manufacturers, who processed it into so-called can sheet to produce new beverage containers. Each of these newly produced aluminum cans contained about 51% recycled metal. Other types of old scrap aluminum often contain other alloyed metals and are thus not used to make beverage containers or aluminum foil but may be sold to aluminum mills for production of other products. 16.7.3.2 Ferrous Metals

There are three types of ferrous metal scrap. Home scrap is produced in steel mills during production of the steel and is recycled internally. Prompt industrial scrap is produced during machining, stamping, and other fabrication processes during the production of iron and steel items. Obsolete scrap consists of iron and steel products that have served a useful purpose and are now being discarded. Railroad cars and tracks, automobiles, and trucks are major sources of obsolete scrap; other sources include manhole covers, old water pipes, lawn mowers, pots and pans, and steel cans. Steel cans can be collected along with aluminum cans because the two types of can can be easily sorted by means of magnetic separation (the steel cans can be magnetized, while the aluminum cans cannot). Steel mills use scrap iron and steel in the manufacture of new steel (Section 12.2.4). The obsolete scrap most often recycled by consumers consists of steel cans that have been used as containers for food, beverages, paint, or aerosols. To protect the contents of the cans from corrosion, these steel cans are usually lined with a very thin coating of tin, about 3  10 5 in. thick. These cans, often called ``tin'' cans, have the tin recovered by detinning companies during recycling. Detinning companies use either a chemical and electrolytic process or heat treatment (tin melts at about 2328C) to remove the tin. The chemical process consists of dissolving the tin as sodium stannate with a sodium

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hydroxide±sodium nitrate solution. In the electrolytic process, the scrap steel is made anodic, and the tin electrolytically dissolved and redeposited on the cathode. Some food cans, including tuna cans, are made with tin-free steel, while some others have an aluminum lid and a steel body (bimetal cans) whose parts can be separated magnetically after shredding. In 1995, almost 56% of steel and bimetal cans in the United States were recycled.

16.7.4 Plastics All plastics are made of polymers, which were discussed in Section 7.3. Although most plastics waste in the United States has been placed in land®lls, Switzerland, Japan, and some other countries, have disposed of most of their plastics waste by incineration. Although the incinerators used include excellent antipollution devices, they have not been accepted by the populations of many countries. Most plastics wastes are not being recycled at this time. For example, the plastics used in some durable goods such as automobiles may consist of mixtures of as many as 50 or 60 different plastics that are not currently being separated for recycling. A number of ways are being found to get around this problem: 1. It is possible to use fewer different plastics in the manufacture of automobiles. 2. Some companiesÐfor example, General ElectricÐhave made long-term agreements with scrap dealers who buy junked automobiles to obtain the plastic parts from these automobiles for recycling. 3. Manufacturers may be asked to put identifying bar codes on each polymer-containing component. 4. Uses can be found for the mixed polymersÐfor example, tiny beads of mixed plastic can be used by the aircraft industry in a process analogous to sand blasting for removing paint from aluminum. Many manufacturers of plastics now attempt as much recycling of plastics wastes produced during production as possible. In the rest of this section, however, we shall be concerned only with the postconsumer plastics waste that has been labeled with the Society of the Plastics Industry (SPI) system shown in Figure 16-5. The six main polymers now labeled for recycling make up most of the postconsumer plastics wastes (numbers 2 through 6 make up about 85% of these). Some municipalities collect mixed plastics wastes, while others collect only plastics wastes that have been separated by number. In 1993 about 7% of the plastics labeled with numbers 1 through 6 in Figure 16-5 were recycled in the United States. In western Europe, in the same year, about 21% of municipal plastics waste was either reused or incinerated in a way that produced useful energy (see Section 16.5).

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Recycling symbol

Polymer

Examples of use Soft drink bottles, carpets, fiberfill, rope, scouring pads, fabrics, Mylar tape(cassette and computer)

Poly(ethylene terephthalate)

1

O C

O

CH2 CH2 O n

PETE* High density polyethylene

2

CH2 CH2

n

Milk jugs, detergent bottles, bags, plastic lumber, garden furniture, flowerpots, trash cans, signs

HDPE Poly(vinyl chloride)

3

CH2 CHCl

n

Cooking oil bottles, drainage and sewer pipes, tile, institutional furniture, credit cards

V Bags, squeeze bottles, wrapping films, container lids

Low density polyethylene

4

CH2 CH2

n

LDPE Yogurt containers, automobile batteries, bottles, carpets, rope, wrapping films

Polypropylene

5

CH2 CH

n

CH3

PP Polystyrene

6

CH2 CH

n

Disposable cups and utensils, toys, lighting and signs, construction, foam containers, and insulation

PS All other polymers

7

Various food containers, hand cream, toothpaste, and cosmetic containers

Other * PETE is used as an abbreviation for poly(ethyleneterephthalate) in recycling codes, but most chemists use the abbreviation PET.

FIGURE 16-5 Recycling codes for plastics.

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16.7 RECYCLING

16.7.4.1 Mixed Postconsumer Plastics Waste

Mixed plastics, after cleaning and shredding, can be melted and extruded under pressure to make ``plastic wood.'' Since most plastics, including those in postconsumer plastics waste, are not miscible with each other, the particles in the ``plastic wood'' do not adhere well to each other, and the material contains voids and often pieces of newspaper, aluminum foil, and anything else that was not removed from the plastics waste before extrusion. The material is thus not very strong and cannot be used under tension; also, the extruded pieces must have a large cross section, several inches or more. Plastic wood is used in agriculture (fences, animal pens, tree supports), marine engineering (seawalls, boat docks, boardwalks, lobster traps), recreational equipment (park benches, picnic tables, stadium seating), gardening (compost bins, garden furniture), civil engineering and construction (signposts, siding insulation, shutters, roof tiles), and for industrial uses (highway construction, pipe racks, traf®c barriers). It is generally more useful to separate the postconsumer plastic waste into its constituent plastics (Figure 16-5), either at the source or after collection. There are many ways to do this; some of these are separation by hand, various ¯otation methods that separate the (shredded) plastics by density, and many other methods that are applicable to particular plastic mixtures. For example, bottles made of poly(vinyl chloride), PVC, can generally be separated from other bottles by using various devices based on the infrared absorption or the ¯uorescence emission of these bottles as contrasted with that of bottles made from other plastics. The bottles are on a conveyor belt; when the sensor detects a PVC bottle, this bottle is ejected from the belt into a special container. Methods based on the different solubility of the various plastics in different solvents or in the same solvent (xylene) at different temperatures are also being considered; in these cases, the polymers must be recovered from the solvents separately. 16.7.4.2 Reuse of Pure Plastics

Most 1- and 2-liter soda bottles are made primarily of poly(ethylene terephthalate), PET, and, in states such as New York State, are recycled separately from other plastic waste; this may be done by imposing a bottle deposit, which is returned to the consumer when the empty bottle is turned in at a collection center. These bottles can be used to produce polyester ®ber, which is used in carpets (in 1995, it was used in 50% of all polyester carpeting sold in the United States), outdoor clothing, insulation, furniture stuf®ng, and so on. Waste nylon is also processed into ®ber to make carpets, tennis ball felt, and other items. High-density polyethylene (HDPE), used for milk and other bottles when ®rst produced, has been recycled for use in non food containers for such

789

16. SOLID WASTE DISPOSAL AND RECYCLING

products as oil, antifreeze, and laundry detergent. It can also be used for drainage pipes, ¯ower pots, trash cans, kitchen drain boards, and so on. Recycled milk jugs have been made into a superior type of plastic wood that is hard to split, easy to saw, colorable while being produced, and stands up better than treated lumber to weather and insects. Although it costs much more than treated lumber, its durability makes it less expensive in the long run. 16.7.4.3 Tertiary Recycling of Plastics

Tertiary recycling is the production of basic chemicals and fuels from plastic waste, as de®ned by the American Society for Testing and Materials (ASTM). The polymers may be chemically decomposed by various methods, or they may be pyrolyzed. Tertiary recycling is used even for polymers that may be recycled as such (see Section 16.7.4.2) because food and drug regulations in the United States forbid the use of melt-process recycled plastics for anything that will contact food. 16.7.4.3.1 Chemical Decomposition of Polymers

Many polymers can be decomposed back into their monomers by using thermal or chemical treatments. These include many more plastics than those few used as illustrations in this section. A number of different chemical companies have treated PET with ethylene glycol, methanol, or water at elevated temperatures under pressure to produce the chemicals from which PET may be resynthesized, dimethyl terephthalate and ethylene glycol. Equation (16-1) shows the methanolysis reaction, which is widely used because it is relatively insensitive to the additives and contaminants that may be included in the recycled polymer. O

O

C

C

O

+ 2n CH3OH

CH2CH2 O n

…16-1†

PET O

O

n CH3O C

C

OCH3 + n HO

CH2CH2 OH

Polyurethanes, used in foam mattresses, foam insulation, and proprietary elastic ®bers such as Spandex, are various polymeric materials that contain urethane, ÐNHCOÐ, groups formed from isocyanates, often aromatic ones, and polyols. When polyurethane foam products are mixed with superheated steam, they liquefy and hydrolyze to the amine corresponding to the starting isocyanate, usually 2,5-diaminotoluene, propylene glycol, and carbon dioxide.

790

16.7 RECYCLING

O

CH3

CHN

O NHCOCH2CH2CH2O + 2n H2O n

[Simplified polyurethane structure]

…16-2†

CH3 n

H2N

NH2

+ 2n CO2 +

n HOCH2CH2OH

Equation (16-2) shows a very simpli®ed structure of a polyurethane. More than one glycol and more than one aromatic diisocyanate may have been used to make the polyurethane and, in addition, parts of the polymer chains may consist of polyesters, polyethers, and polyamides. Therefore, additional low molecular weight compounds are usually produced by hydrolysis. Alcoholysis using a short-chain alcohol has also been used to decompose polyurethanes; in this case, no carbon dioxide is formed. The low molecular weight compounds produced can be mixed with diisocyanates and new foamed polyurethanes can be produced. Nylon 6 can be depolymerized at high temperature or by using various hydrolysis reactions to form the monomer, which can be puri®ed and repolymerized: NH

(CH2)5 CO Nylon 6

n

CH2

C H2

CH2

CH2

C H2

CO

NH

…16-3†

Caprolactam

16.7.4.3.2 Pyrolysis

Pyrolysis is the thermal fragmentation of plastics into small molecules, either in the absence of oxygen or in an oxygen-de®cient atmosphere, at temperatures as high as 500±10008C. Waste items made of a single polymer, a mixture of polymers, or, for that matter, mixed household wastes, may be and have been pyrolyzed. Gases, liquids, and solids are obtained. The gases obtained may include CO, CO2 , H2 , CH4 , ethylene, propylene, and others. Some of these gases are used to heat the pyrolysis plant so that no external energy source is needed for this purpose. The liquids that are formed include benzene, toluene, naphthalene (this is dissolved in the other liquids), fuel oil, and kerosene, depending on the plastics that are pyrolyzed. The solids obtained are mostly carbon black and waxes (these are hydrocarbons). Figure 16-6 shows a schematic of a pyrolysis plant using a ¯uidized bed of sand.

791

16. SOLID WASTE DISPOSAL AND RECYCLING

Plastics waste

Fluidized bed reactor

Carbon black separation Burner effluent gas

Carbon Distillation column

Fluidized sand 600−900 C Burner

Fluidized gas (pyrolysis gas)

Gas cooling at 30−40 C Heating

50% for heating the plant and fluidizing gas (methane, ethylene, propylene) 50% as an end product

Pyrolysis gas separated into benzene, toluene, wax, etc.

FIGURE 16-6 A ¯uidized-bed reactor for the pyrolysis of plastic waste. From N. Mustafa, ed., Plastic Waste Management: Disposal, Recycling, and Reuse by courtesy of Marcel Dekker, Inc. Copyright # 1993.

Additional Reading Andrews, G. D., and P. M. Subramanian, eds., Emerging Technologies in Plastics Recycling. American Chemical Society, Washington, DC, 1992. Bagchi, A., Design, Construction and Monitoring of Land®lls, 2nd ed. Wiley, New York, 1994. Brandrup, J., M. Bittner, W. Michaeli, and G. Menges, eds., Recycling and Recovery of Plastics. Hanser=Gardner, Cincinnati, OH, 1995. Diaz, L. F., G. M. Savage, L. L. Eggerth, and C. G. Golueke, Composting and Recycling Municipal Solid Waste. Lewis Publishers, Boca Raton, FL, 1993.

792

ADDITIONAL READING

Haug, R. T., The Practical Handbook of Compost Engineering. Lewis Publishers, Boca Raton, FL, 1993. Kreith, F., ed., Handbook of Solid Waste Management. McGraw-Hill, New York, 1994. Lund, H. F., ed., The McGraw-Hill Recycling Handbook. McGraw-Hill, New York, 1993. Manser, A. G. R., and A. A. Keeling, Practical Handbook of Processing and Recycling Municipal Solid Waste. Lewis Publishers, Boca Raton, FL, 1996. Mustafa, N., ed., Plastics Waste Management: Disposal, Recycling, and Reuse. Dekker, New York, 1993. Niessen, W. R., Combustion and Incineration Processes, 2nd ed. Dekker, New York, 1995. Polprasert, C., Organic Waste Recycling, 2nd. ed. Wiley, Chichester, 1996. Strong, D. L., Recycling in America. ABC-CLIO, Santa Barbara, CA, 1997. Wilson, D. J., and A. N. Clarke, Hazardous Waste Site Soil Remediation. Dekker, New York, 1994.

APPENDIX A

Designation of Spectroscopic States

A.1 INTRODUCTION The recipes brie¯y summarized here are used in arriving at atomic and molecular state (energy) descriptions. The reader is referred to standard textbooks of quantum mechanics and spectroscopy, some of which are given in the Additional Reading, for the mathematical formulations of these principles. A.2 ATOMS The state of the electron in the hydrogen atom or hydrogen-like ion (e.g., He‡ and Li2‡ , each containing only one electron) is speci®ed by the three quantum numbers n, l, and ml . The principal quantum number n can have the values 1, 2, 3, . . . ; it de®nes the shell of the atom occupied by the electron, and therefore the total energy of the single bound electron (neglecting relativistic effects) is speci®ed completely by n. The azimuthal or orbital angular momentum quantum number l can have the values 0, 1, 2 . . . (n 1); it determines the total angular momentum of the electron, which is quantized and can be represented by a vector having magnitudes …h=2
†‰l…l ‡ 1† Š1=2 (where h is Planck's constant). The states (or atomic orbitals) with l ˆ 0, 1, 2, 3, . . . are designated, respectively, s, p, d, f, . . . orbitals, so that the electron in the lowest electronic state of the hydrogen atom (n ˆ 1, l ˆ 0) is called a 1s electron. The quantum number ml is the magnetic quantum number (so named because it is related to the effects of a magnetic ®eld on atomic spectra), and can have the values l, …l 1†, . . . , 0, . . . (l 1), l; it determines the allowed components of the angular momentum in a de®nite z direction, which are also quantized and can only have values of ml h=2
. 793

794

DESIGNATION OF SPECTROSCOPIC STATES

In addition to the three quantum numbers given, another factor, electron spin, must be considered to explain the ®ne structure observed in atomic spectra. This fourth parameter is also a natural consequence of quantum mechanics if relativistic effects are included in the detailed wave mechanical treatment. In addition to orbital angular momentum described by the quantum number l, an electron has an intrinsic magnetic moment as if (classically) it were spinning about its own axis in addition to orbiting the nucleus. Associated with this moment is a quantum number s, such that the total spin angular momentum vector has a magnitude …h=2
†‰s…s ‡ 1†Š1=2 ; however, s can have only the single value of 1=2. Analogous to the orbital angular momentum, the z component of the spin angular momentum is also quantized with allowed values of magnitude ms h=2
, where ms ˆ 1=2 (so that there are only two possible orientations of the spin angular momentum). The electron spin and orbital angular momentum magnetic moments interact, so that l and s are coupled to give a total electronic angular momentum vector of magnitude h=2
‰ j…j ‡ 1†Š1=2 where j ˆ l  s ˆ l  1=2. With polyelectronic atoms, the complexities of the mathematics involved in describing the system as a result of electrostatic interactions among the electrons as well as between the electrons and the nucleus are such that only approximate solutions of the quantum mechanical treatment are possible. The concept of hydrogen-like orbitals is retained with the principal quantum number n designating the electronic shells of the atom, but now the energy of the state is a function of the total angular momentum of the electrons as well as the quantum number n. The number of electrons in a given orbital is governed by the Pauli exclusion principle, which states that no two bound electrons can exist in the same quantum state; that is, no two electrons in the atom can have the same values of n, l, ml , and ms . Thus, an atomic orbital characterized by a speci®c set of n, l, and ml values can be occupied by two electrons only if their spins are opposed with ms ˆ ‡1=2 and 1=2. Subject to this constraint, the orbitals are ®lled in the order of increasing energy (the aufbau principle). If two or more orbitals have the same energy (i.e., are degenerate), then the electrons go into different orbitals as much as possible, thus reducing electron±electron repulsion by keeping them apart, with spins parallel and in the same direction rather than opposed (Hund's rule). For light atoms of the type we shall be concerned with here (nuclear charge < 40), the orbital angular momenta of all the electrons strongly couple together to give a total, or resultant, orbital angular momentum. This is designated by the quantum number L, which is obtained by the combination of the moments of the individual electrons. Similarly, the spin angular momenta combine to give a resultant spin, designated by the quantum number S. It follows that the total orbital angular momentum in the z direction is characterized by a quantum number ML ˆ ml, and the total spin angular momentum in the z direction has associated with it a quantum number MS ˆ ms.

795

APPENDIX A

Allowed values of ML are L, …L 1†, . . . , 0, . . . , (L 1), L (i.e., jML j  L) and allowed values of MS are S, …S 1†, . . . , 0, . . . , …S 1†, S …or jMS j  S†. Closed (completely ®lled) shells and subshells have to a good approximation zero net resultant orbital and spin angular momenta, so that the combination need be carried out over only the electrons in partially ®lled subshells. Examples of this process are given later. The L and S momenta then couple together (Russell±Saunders coupling) to form a total atomic angular momentum J. Possible values of J are J ˆ L ‡ S, L ‡ S

1, L ‡ S

2, . . . , jL

S ‡ 1j, jL

Sj

…A-1†

where jL Sj is equal to L S, if L  S, and equals S L if S  , L (i.e. , J can only have positive values). The complete term symbol, which designates the electronic state of the atom, is written n 2S‡1LJ

…A-2†

Frequently, n is omitted. The quantity (2S ‡ 1) is the multiplicity of the atom (called singlet, doublet, triplet, etc., respectively, for values of 1, 2, 3, . . . ); it gives the total number of possible spin orientations. Often the value of J is omitted from the term symbol, particularly if the energy differences among the different J states are so small that they are not a factor in photochemical considerations. Analogous to hydrogen or hydrogen-like atoms, the atomic states of L ˆ 0, 1, 2, 3, are designated, respectively, S, P, D, F, states. As a speci®c example, consider the oxygen atom with eight electrons in an electronic con®guration 1s2 2s2 2p4 . The 1s shell and the 2s subshell are completely ®lled, hence only the four 2p (l ˆ 1) electrons need be considered. The state of lowest energy, hence the most stable, is called the ground state. According to Hund's rules, this state is the state of maximum multiplicity; for a given multiplicity, the state of maximum L; and for given L and S, the state of minimum J if the partially ®lled subshell is less than half-occupied, or conversely, the state of maximum J if the partially ®lled subshell is more than half-occupied. Thus the ground state of oxygen is given by the four electrons occupying the three 2p orbitals in the following manner:

The quantum numbers for the four electrons in this un®lled p subshell are as follows: Electron

n

l

ml

ms

1 2 3 4

2 2 2 2

1 1 1 1

‡1 ‡1 0 1

‡1=2 1=2 ‡1=2 ‡1=2

796

DESIGNATION OF SPECTROSCOPIC STATES

For this con®guration MS is Sms ˆ 1=2 1=2 ‡ 1=2 ‡ 1=2 ˆ 1, which is the maximum possible for 4 electrons in 3 orbitals to be consistent with the Pauli exclusion principle, and therefore S ˆ 1 ( since jMS j  S) and the multiplicity …2S ‡ 1† ˆ 3. Similarly, ML ˆ ml ˆ 1, which is also the maximum possible value; hence L must also be 1, since jML j  L. The quantities S and L are maximum allowed values, and therefore they give the state of lowest energy which is a 23 P (a ``triplet-P'') state. Possible J values are 2, 1, and 0; since the subshell is more than half-®lled, maximum J gives the most stable state, and therefore the complete term symbol for the oxygen atom in its lowest energy state is 23 P2 . Electronic excitation may result in change of J (generally unimportant in photochemistry, an exception being the rather large separations between the halogen 2 P3=2 and 2 P1=2 states), transition to another orbital within the subshell, or transition to a higher energy subshell. For example, two possible excited states of the oxygen atom within the same subshell (same n ˆ 2 and l ˆ 1) are as follows: "# ml ms

‡1, ‡ 1 ‡1=2, 1=2

"# 0, 0 ‡1=2,

1=2

and "# ml ms

‡1, ‡ 1 ‡1=2, 1=2

"# 1, 1 ‡1=2, 1=2

The term symbols are 21 D2 and 21 S0 , respectively, the former being of lower energy because of maximum L. Similarly, it can readily be veri®ed using the same procedure that the total momenta for nitrogen with seven electrons (1s2 2s2 2p3 ) in the ground-state con®guration is S ˆ 3=2 (multiplicity ˆ 4), L ˆ 0, and J ˆ 3=2; hence the term symbol is 24 S3=2 . A possible excited state is 22 D3=2 . It should be pointed out that some excited electronic con®gurations are excluded by the Pauli exclusion principle for atoms with electrons with the same values of n and l (called equivalent electrons), because simply interchanging the order in the designation does not lead to different states.

A.3 DIATOMIC MOLECULES For diatomic (or linear polyatomic) molecules, it is possible to designate the electronic states by a set of quantum numbers analogous to atoms. Thus, electrons with atomic orbital angular momentum quantum number l can

797

APPENDIX A

have quantized molecular values l from 0 to l, and these combine in a manner analogous to polyelectronic atoms to give a quantum number L representing the total orbital angular momentum along the internuclear axis. It is possible for L to have values 0, 1, 2, . . . , L (where L is the quantum number for the resultant orbital angular momentum for all the electrons in the molecule), and these are designated, respectively, S, P, D, . . . states, analogous to s, p, d, . . . , for the hydrogen atom and to S, P, D, . . . for polyelectronic atoms. Similarly, the total molecular spin quantum number is S, and the component of S along the internuclear axis is S with possible values S, S 1, . . . , 0, …S 1†, S. The sum of these two quantum numbers is a quantum number analogous to J, V ˆ jL ‡ Sj, and the total term symbol for a speci®c diatomic or linear polyatomic electronic state is …2S‡1†

…A-3†

LV

In addition to these quantum numbers L, S, and V, there are two other properties of homonuclear diatomic species dealing with the symmetry of its wave function: 1. If inversion of all electrons through a center of symmetry of the molecule leads to no change in sign of the electronic wave function, then the state is even, or gerade (g); if a change of sign results, the state is odd, or ungerade (u). The symbol g or u is included in the molecular term symbol as a second subscript to L. 2. If re¯ection in a plane of symmetry passing through the nuclei (containing the internuclear axis of symmetry) leads to no change in sign of the electronic wave function; then the state is positive (‡); if it changes sign, the state is negative (±) . The symbol ‡ or ± is written as a second superscript to L. (This element of symmetry applies only to L ˆ 0 or S states.) Molecular oxygen provides a practical atmospheric photochemical example for illustrating these state designation factors. The electronic con®guration for ground-state O2 (16 electrons) is …sg 1s†2 …
u 2py †2

…su 1s†2

…sg 2s†2

…
g 2px †1

…su 2s†2

…sg 2pz †2

…
u 2px †2

…
g 2py †1

The (g 1s), and so on designate molecular orbitals, the asterisk (*) refers to an antibonding orbital (i.e., the density of electrons between the two oxygen atoms in this type of orbital is less than that for the two free atoms, and therefore there is a repulsive force between them), and the superscript gives the number of electrons in the molecular orbital. Since there are two unpaired electrons in the equivalent (degenerate) (
g 2px ) and (
g 2py ) orbitals, by Hund's rule of maximum multiplicity the total spin is 1 and the ground state

798

DESIGNATION OF SPECTROSCOPIC STATES

is a triplet. The quantum number L can be 2 or 0; however, if L ˆ 2, both electrons would have the same l ˆ 1 value, which is forbidden by the Pauli exclusion principle for electrons in equivalent orbitals also with the same spins; therefore only the L ˆ 0, or S, state is allowed for S ˆ 1. Figure A-1 shows the wave functions for one of the two unpaired electronsÐthe one in the (
g 2px ) orbitalÐfor the lowest energy con®guration, from which it is seen that interchange through the center of symmetry does not lead to a change in sign, whereas interchange through the plane of symmetry does. The ground state of oxygen is therefore gerade and negative, and the term symbol is 3 g . While the ground electronic state of O2 is the 3 g state, there are two other possible states (of somewhat higher energies) for the electrons in these same two equivalent orbitals in which the total spin is zero (multiplicity ˆ 1). In this case, both electrons can now have either the same  values (each ‡1 or 1), leading to  ˆ 2 and a 1  state, or different  values (‡1 and 1) giving a net angular momentum component  ˆ 0 and hence a 1  state. From the same symmetry considerations based on Figure A-1 that were used to obtain the term symbol for the ground state, it follows that the term symbols for these two electronically excited states are 1 g and 1 ‡ g . On the other hand, if an electron in a lower energy orbital [such as the (
u 2py ) state] is excited to the

X +

−

P

C

Z

P9 +

P0 − Y

FIGURE A-1 Schematic drawing of the (
g 2px ) orbital of O2 in the X Z plane, the plane of the page. [The (
g 2py ) orbital, not shown, is in the y z plane perpendicular to the plane of the page.] Inversion through the center of symmetry C from P to P0 does not change sign, whereas inversion through a plane of symmetry passing through the two nuclei such as the y z plane (from P to P00 ) does lead to a change in sign.

799

APPENDIX A

(
g 2py ) orbital, then two nonequivalent orbitals, (
u 2py ) and (
g 2px ), are singly occupied; the Pauli exclusion principle no longer applies, since the two unpaired electrons occupy separate orbitals, and six states are possible: 1 ‡ 1 3 3 u , u , 1 u , 3 ‡ u , u , and u .

A.4 POLYATOMIC MOLECULES Although the concepts developed for atoms and diatomic species can be extended to polyatomic molecules, the designation of electronic states for more complex molecules can become quite complex if the maximum spectral information is to be retained. However, many of the more subtle points that are especially important for ®ne-structure spectroscopic characterizations in most cases simply do not affect understanding of photochemical transformations involving complex species, and therefore for our purposes we can get by with relatively simple terms involving orbitals for only a single optical electron. The optical electron is the one electron promoted in the light absorption process. Of importance for these orbitals are their symmetry and multiplicity characteristics, plus their involvement in bonding within the molecule. These may be of the following types involving both bonding and antibonding characteristics: 1.  and  orbitals: these are associated with two atoms and involve two tightly bound electrons 2.
and
 orbitals: for example, the contribution of p electrons to the double bond in ethylene, or the conjugated electrons in benzene 3. n orbitals: these are nonbonding orbitals occupied by lone pair electrons in heteroatomic molecules Excited states are then designated by the initial and ®nal orbitals associated with the transition of the optical electron. Thus, the ®rst excited state of ethylene is formed by promoting an electron from a bonding
orbital to an antibonding
 orbital, leading to two unpaired electrons. Hund's rule of maximum multiplicity again suggests the spins of these electrons should be in the same direction, so that S ˆ 1 and the multiplicity is 3. The designation of this state is 3 …
,
 †. For a molecule involving a carbonyl group, R C O R9

an additional low-lying state is the 3 …n,
 † state formed by exciting an electron from the nonbonding n orbital to the antibonding
 orbital. The state of lower energy, whether the 3 …n,
 † or the 3 …
,
 † state, will depend somewhat

800

DESIGNATION OF SPECTROSCOPIC STATES

on substituent (R and R ) groups and on the physical environment of the molecule.

Additional Reading Harmony, M. D., Introduction to Molecular Energies and Spectra. Holt, Rinehart, & Winston, New York, 1972. Herzberg, G., Atomic Spectra and Atomic Structure, 2nd ed. Dover, New York, 1974. Herzberg, G., Spectra of Diatomic Molecules. Van Nostrand, Princeton, NJ, 1950. Herzberg, G., Electronic Spectra and Electronic Structure of Polyatomic Molecules. Van Nostrand, Princeton, NJ, 1966. Karplus, M., and Porter, R. N., Atoms and Molecules. W. A. Benjamin, New York, 1970. McQuarrie, D. A., and Simon, J. D., Physical Chemistry: A Molecular Approach. University Science Books, Sausalito, CA, 1997.

APPENDIX B

Thorium and Actinium Series

TABLE B-1 Thorium (4n) Series Nuclidea

Z 232

90 90 89 88 88 86 84 84 83 82 82 81

Th (Th) Th (RdTh) 228 Ac MsTh2  228 Ra MsTh1  224 Ra ThX 220 Rn (Tn) 216 Po (ThA) 212 Po ThC0 † 212 Bi (ThC) 212 Pb (ThB) 208 Pb (ThD) 208 Tl …ThC00 † 228

Radiationb

Half-life 1
405  1010 y 1.913 y 6.15 h 5.76 y 3.66 d 55.6 s 0.145 s 298 ns 1.009 h 10.64 h Stable 3.053 m

a a, b b a, a a a a, b

(g) ,g (g)

35.9%; b , 64.1%, g ,g

b ,g

a

Symbol used in the early studies of naturally occurring radioactivity is given in parentheses: …MsTh1 †, mesothorium I; (RdTh), radiothorium; (Tn), thoron. b (g) indicates low intensity (1±5%); g rays with intensity below 1% are not included. Where both a and b are given, branched decay occurs.

801

802

THORIUM AND ACTINIUM SERIES

232

90 (Th)

228 228

89 (Ac) 228

88 (Ra)

224

87 (Fr)

–

86 (Rn)

220

85 (At) 216

84 (Po) 83 (Bi)

212 212

212

82 (Pb) 81 (Tl)

208 (s) 208

FIGURE B-1 Thorium (4n) series. The main sequence is indicated by arrows and a dash.

TABLE B-2 Actinium (4n  3) Series Nuclidea

Z 92 91 90 90 89 88 87 86 85 85 84 84 83

235

U (AcU) Pa (Pa) 231 Th (UY) 227 Th (RdAc) 227 Ac (Ac) 223 Ra (AcX) 223 Fr (AcK) 219 Rn (An) 219 At (At) 215 At (At) 215 Po (AcA) 211 Po …AcC0 † 215 Bi (Bi) 231

Half-life 7
04  108 y 3
28  104 y 1.063 d 18.72 d 21.774 y 11.435 d 21.8 m 3.96 s 56 s 0.10 ms 1.780 ms 0.516 s 7.6 m

Radiationb a, g a, (g) b ,g a, g b , 98.62%; a, 1.38% a, g b , 99‡ %, g; a,  0
005% a, g a,  97%; b ,  3% a a, 99%; b , 3
3  10 4 % a b (continues)

803

APPENDIX B

TABLE B-2 (continued ) Z

Nuclidea 211

83 82 82 81

Bi (AcC) Pb (AcB) 207 Pb (AcD) 207 Tl AcC00 †

211

Half-life 2.14 m 36.1 m Stable 4.77 m

Radiationb a, 99.72%, g b ,g b

a

Symbol used in the early studies of naturally occurring radioactivity is given in parentheses. (AcU), actinouranium; (RdAc), radioactinium; (An), actinon. b (g) indicates low intensity (1±5%); g rays with intensity below 1% are not included. Where both a and b are given, branched decay occurs.

92 (U)

235 231

91 (Pa) 90 (Th) 89 (Ac)

231

227

227 −

88 (Ra) 87 (Fr)

223

223

86 (Rn) 85 (At)

219

219

84 (Po) 83 (Bi) 82 (Pb) 81 (Tl)

215 211

215

215

211

211

207 (s) 207

FIGURE B-2 Actinium (4n ‡ 3) series. The main sequence is indicated by arrows and a dash.

APPENDIX C

Units

SI Units Quantity

Unit

Symbol

Amount of substance Electric current Energy Length Mass Power Pressure Radioactive decay Temperature Time

mole ampere joule meter kilogram watt (1 J=s) pascal becqerel kelvin second

mol a J m kg W Pa Bq K s

Pre®xes Name

Symbol

Multiplying factor

atto femto pico nano micro milli centi deci deka hecto kilo mega giga tera peta exa

a f p n m m c d da h k M G T P E

10
18 10
15 10
12 10
9 10
6 10
3 10
2 10
1 10 102 103 106 109 1012 1015 1018

805

806

UNITS

Derived Units Name and symbol

Value

acre Ê) angstrom (A atmosphere (atm) bar barrel (petroleum) ˆ 42 gal ˆ 306 lb calorie (cal) curie (Ci) electron-volt (eV) foot (ft) gallon (gal) hectare metric tonÐsee tonne mile (mi) ton (U.S. long); 2240 pounds ton (U.S. short); 2000 pounds tonne (metric ton); 2205 pounds

0.4047 hectare 10
10 m or 0.1 nm 101325  105 Pa 105 Pa 0159 m3 4184 J 370  1010 Bq 1602  10
19 J 0.3048 m 3786  10
3 m3 104 m2 1609344 m 1016  103 kg 9072  102 kg 1  103 kg

APPENDIX D

Symbols and Abbreviations

Note: Some of these symbols have other meanings when used in speci®c contexts; other symbols that are used only in speci®c contexts may not be included. a b g D e e0 Z l L mat ne ne s t T f F 2,4-D 2,4,5-T A A AÊ ABS amu atm

Earth's albedo (re¯ectivity); also Beer±Lambert proportionality constant; also alpha particle Beta particle Gamma rays Difference or change in a quantity Extinction coef®cient; also ef®ciency of a fuel cell Permittivity in vacuum Ef®ciency Wavelength; also nuclear decay constant Orbital angular momentum quantum number (along internuclear axis) Attenuation coef®cient for g rays Frequency; also kinetic rate; also symbol for electron neutrino Electron, antineutrino Absorption cross section, also nuclear reaction cross section Mean-life Residence time Primary quantum yield Overall quantum yield 2,4-dichlorophenoxyacetic acid 2,4,5-trichlorophenoxyacetic acid Ampere; electric current Activity (in radioactive decay); also mass number; also Arrhenius preexponential factor AÊngstrom Alkylbenzenesulfonates Atomic mass unit Atmosphere

807

808

SYMBOLS AND ABBREVIATIONS

BOD Bq Btu BWR c C C CAFE cal CFC Ci COD Cp CTBT D DDE DDT DNA DOC DOE DU E Ea EC ECCS EDTA Eg EH E EPA eV exp F ft g G gal GWP Gy h H HC HCFC HEU HFC HFE HLW HWR I IC ILW

Biological oxygen demand Becquerel (1 disintegration per second) British thermal unit (1 054 J) Boiling water reactor Speed of light in vacuum (2
998  108 m=s) Coulomb; also Celsius (as in 8C) Concentration Corporate average fuel economy Calorie Chloro¯uorocarbon Curie; 3
7  1010 disintegrations per second Chemical oxygen demand Heat capacity at constant pressure Comprehensive Test Ban Treaty Dose of ionizing radiation Dichlorodiphenylethylene; 1,1-dichloro-2,2-bis(p- chlorophenyl)ethylene Dichlorodiphenyltrichloroethane; 1,1,1-trichloro-2,2- bis(p-chlorophenyl)ethane Deoxyribonucleic acid Dissolved organic carbon U.S. Department of Energy Dobson unit Energy; potential Arrhenius activation energy Electron capture (nuclear process) Emergency core cooling system (nuclear reactor) Ethylenediaminetetraacetic acid Band gap Cell potential on the hydrogen scale Standard potential U.S. Environmental Protection Agency Electron-volt Exponential; exp(y)  ey Faraday constant, 96,485 coulombs Foot Gram; also molecular symmetry designation, gerade (even) Free energy; Gibbs function Gallon Global warming potential Gray  100 rads Planck's constant (6
626
1034 J  s) Enthalpy (not to be confused with the symbol for hydrogen, roman H) Hydrocarbon Hydrochloro¯uorocarbon High enrichment uranium Hydro¯uorocarbon Hydro¯uoroether High-level waste (radioactive) Heavy water reactor Radiation intensity Internal conversion (nuclear process) Intermediate-level waste (radioactive)

809

APPENDIX D

IT J J k K K Ka Kb keV kg Ksp Kw L LAS LD50 LET LEU LLW LMFBR LOCA LWBR LWR m M MeV MH mi mol MON MOX MRI MTBE MTHM MWd MWe MWt N NA NOx NPT NRC ODP p P Pa PBB PCB pE PET PFC

Isomeric transition (nuclear process) Joule Total angular momentum quantum number of an atom Boltzmann constant (1
381  10 23 J molecule 1 K 1 ); also rate constant Kelvin Equilibrium constant Acid dissociation (ionization) constant Base dissociation (ionization) constant Thousand electron-volts Kilogram Solubility product constant Ion product of water Net electronic orbital angular momentum quantum number Linear alkylsulfonates Lethal dose for 50% of the population Linear energy transfer Low-enrichment uranium Low-level waste (radioactive) Liquid metal fast breeder reactor Loss of coolant accident (nuclear reactor) Light water breeder reactor Light water reactor Meter, mass Molarity (mol=dm3 ) Million electron volts Metal hydride Mile Mole of substance Motor octane number Mixed oxide (Pu and U oxides) Magnetic resonance imaging Methyl t-butyl ether Metric ton of heavy metal Megawatt-day Megawatts of electricity Megawatts of heat (t ˆ thermal) Neutron number, also number of atoms Avogadro's number; 6
023  1023 particles Nitrogen oxides Non-Proliferation Treaty U.S. Nuclear Regulatory Commission; also National Research Council Ozone depletion potential Proton Pressure Pascal Polybrominated biphenyl Polychlorinated biphenyl Negative log of electron activity (a measure of redox potential) Poly(ethylene terephthalate); also position emission tomography Per¯uorocarbon

810

SYMBOLS AND ABBREVIATIONS

pH pK POC ppb ppbv ppm ppt pptv PSC PVC PWR q Q Q r R R rad RBE RBMK rem RON s S SNF Sv T t1=2 Tc TCDD Teff TMI TOC TRU u U UV UV-A UV-B UV-C V V VOC w W WL wR wT Z Z

Negative log of H activity (approx. concentration) ±log K Particulate organic carbon Parts per billion Parts per billion by volume Parts per million Parts per trillion Parts per trillion by volume Polar stratospheric cloud Poly(vinyl chloride) Pressurized water reactor Heat; also electric charge Quad (1
054  1018 J) Energy in nuclear reactions; also quality factor (for ionizing radiation) Rate of reaction Roentgen Universal gas constant (8
314 J  K 1 mol 1 ) Radiation absorbed dose (10.0 mJ=kg) Relative biological effectiveness Reactor high-power boiling channel nuclear reactor (Soviet) Roentgen-equivalent man (a measure of radiation dose) Research octane number Second; also spin quantum number for an electron The solar constant; also used for entropy and net spin angular momentum of an atom Spent nuclear fuel Sievert, dose equivalent (ionizing radiation) Absolute temperature (K) Half-life Critical temperature 2,3,7,8-Tetrachlorodibenzodioxin Effective half-life Three Mile Island Total organic carbon Transuranic waste Molecular symmetry designationÐungerade (odd) Internal energy Ultraviolet radiation;  400 nm Radiation in the range 400±320 nm Radiation in the range 320±290 nm Radiation in the range 290±200 nm Volts Volume, potential energy Volatile organic compound Work Watts Working level (for exposure to a particles from radon progeny) Radiation weighting factor Tissue weighting factor Collision frequency; also atomic number Speci®c collision frequency

INDEX

A Abbreviations, 807±810 Acetylcholine, 273 Acid±base reactions, aqueous media, 306±319 autoionization, 306±307 carbonic acid, 308, 311±317 overview, 307±311 pH, 310±311, 317±319 solubility, 317±319 Acid mine drainage, 386 Acid rain description, 422±425 distribution, 424±425 environmental effects, 20 Acrylonitrile, Orlon synthesis, 210±211 Actinium, decay series, 802±803 Acyl radicals, tropospheric reactions, 138±139 Adsorption mechanisms, in aqueous media colloid properties, 340±341 ion exchange, 341±343 Age determination, radiometric methods, 582, 585±590 Agent orange, toxicity, 269±270 Air pollution, see also speci®c pollutants Clean Air Act, 176, 178, 182 clean up procedures carbon monoxide, 172, 175±176, 178 lead, 172 nitrogen oxides, 172, 175±177, 369 ozone, 172, 240±241 particulates, 172, 182 sulfur dioxide, 172, 374±375

urban centers, 180±181 hydrocarbon sources, 170±181 automobiles, 168±175 catalytic converter effects, 175±177 gasoline additives, 177±179 smog photochemistry characteristics, 3, 126±129, 140±142 nitrogen oxides volatile organic compound absence, 129±135 volatile organic compound presence, 127±129, 135±140 urban atmospheres, 129, 135±140 temperature inversions, 65±69 urban centers, 179±182 low-emission automobiles, 181±182 reduction plans, 180±181 smog photochemistry, 129, 135±140 ALARA concept, ionizing radiation regulatory limits, 659±661 Albedo, climate change effects, 47±48, 59±61 Alcohol ethoxylates degradation, 203±204 synthesis, 200±201 Aldehydes formation, dichloromethane degradation, 234 tropospheric reactions, 133±134, 141 Aldrin environmental degradation, 263±264 synthesis, 260±261 Al®sols, 467







Algal blooms metal complexes, 335 zeolites role, 197 Alkaline earth metals, 382±383 Alkalinity, 316±317, 441 Alkanes, tropospheric reactions, 141 Alkoxy radical, tropospheric reactions, 137±138 Alkyl benzene sulfonates degradation, 203 synthesis, 194, 198±200, 202 Alkylperoxy radical, tropospheric reactions, 137±138 Alkyl radical, tropospheric reactions, 137±138 Alkylsulfonates degradation, 203, 205 synthesis, 198±199 Alpha radiation, see also Ionizing radiation decay energetics, 514±515 dose rate estimation, 547 interaction with matter, 523±524 Aluminosilicates asbestos, 444, 477±481 clays, 464± 466, 474 Aluminum abundance, 446 biological role, 348, 399±400 drinking water standards, 426 environmental sources, 348 half-life, 564 ocean composition, 417±420 recovery from ore, 451, 458±459 recycling, 785 toxicity, 348, 400 Ammonia atmospheric concentration, 16, 21, 95 drinking water standards, 426 in fertilizers, 366±367 properties, 362±370 Amosite, 478 Amphibole, 444 Anaerobic systems biological waste digestion, 777 natural water systems, 439±440 polychlorinated biphenyl biodegradation, 250±251 Androgen, haloorganic compound effects, 235±237 Anorthite, 444 Antarctic ozone hole, photochemistry, 117±121, 241

Antimony biological role, 351 drinking water standards, 426 environmental sources, 351 toxicity, 351 Apatite, 444 Aqueous media acid±base behavior, 306±307 acid±base reactions, 306±319 autoionization, 306±307 carbonic acid, 308, 311±317 overview, 307±311 pH, 310±311, 317±319 solubility, 317±319 adsorption, 341±343 colloidal materials, 340±341 coordination chemistry, 324±340 complexing applications, 333±335 lability, 330±333 in natural systems, 335±339 stability, 330±333 coordination number, 325±327 description, 324±325 geometry, 325±327 metal±ligand preferences, 327±329 water as a ligand, 329±330 ion exchange, 341±343 oxidation±reduction processes, 320±324 temperature and pressure effects, 319±320 water environments acid±base behavior, 306±307 solubility, 303±306 water cycle, 295±297 water properties, 298±303 Aquifers, 296±297 Aragonite, 444 Arctic ozone hole, photochemistry, 121±122 Argon atmospheric concentration, 16 radiometric age determination, 587, 590 Aridsols, 467±469 Arochlors, see Polychlorinated biphenyls Arrhenius equation, 85±86 Arsenic biological role, 350, 405±407 drinking water standards, 406, 426 environmental sources, 350, 406 resistance, 276 toxicity, 350, 405±407 Asbestos, 444, 477±481





Atmosphere, see also speci®c components carbon cycle, 354±362, 463 characteristics atmospheric windows, 45±46, 57, 108, 109 circulation patterns, 15, 30±35 pressure pro®le, 26±30 solar radiation absorption, 40±47 temperature pro®le, 26±30, 104 composition, see also speci®c constituents evidence, 20±21 gaseous constituents, 15±20 particulate constituents, 24±26 general theories, 20±21 isotope fractionation, 584 natural radioactivity sources, 568±578 outdoor air, 568±570 radon in mines and buildings, 570±578 overview, 13±15, 35±36 photochemistry, 91±145 overview, 91±93 troposphere reactions, 126±142 nitrogen oxides, 127±129, 135±140 smog characteristics, 3, 126±129, 140±142 urban atmospheres containing volatile organic compounds, 127±129, 135±140 upper atmosphere reactions, 93±126 nitrogen, 93±95 oxygen, 95±100 ozone, 100±125, 247±248 water, 125±126 sulfur cycle, 370±375 Atomic nuclei, 484±489 Atoms, spectroscopic state designations, 793±796 Autoionization, acid±base behavior in aqueous media, 306±307 Automobiles catalytic converter effects, 175±177 corporate average fuel economy, 174±175 gasoline additives, 177±179 hybrid vehicles, 182 hydrocarbon sources, 168, 170±175 internal combustion engines, 168±170 low-emission automobiles, 181±182 Azinphosmethyl, resistance, 276

Bacteria biodegradation

biological oxygen demand, 206 polymers, 214, 217±218 insect control, 283±285 ore mining, 456 radiation resistant, 604 Barium biological role, 351, 382±383 decay scheme, 508 drinking water standards, 426 environmental sources, 351 toxicity, 351, 382, 632 Basalt, 444 Bateman equation, 498 Batteries, energy storage, 744±750 Bauxite, 444 Beer's law, 80±82 Bene®cation, ore treatment, 454±455 Benzene, surfactant synthesis, 194, 198 Benzo-(a)-pyrene, incineration by-product, 778 Bergius process, coal conversion to hydrocarbons, 188±189 Beryllium biological role, 348, 382±383 drinking water standards, 426 environmental sources, 348, 383 toxicity, 348, 383 Beta radiation, see also Ionizing radiation decay energetics, 508±514 electron capture, 513±514 negatron emission, 508±511 positron emission, 511±513 dose rate estimation, 546±547 interaction with matter, 522±523, 524±528 Biodegradation biological oxygen demand, 206 latex, 207 polychlorinated biphenyl, 250±251 polymers, 214, 217±218 Bio¯avonoids, estrogenic effects, 238 Biogas, anaerobic digestion of biological wastes, 777 Biological oxygen demand biodegradable organic compounds, 206 sewage treatment, 434 Biomass costs, 738 solar energy utilization, 711±713 Bioremediation oil spills, 162±163 soil contamination, 472±473





Birds crude oil effects on marine life, 165±166 plastic refuse effects, 213±214 polychlorinated biphenyl toxicity, 255±256 1,1,1-trichloro-2,2-bis(p-chlorophenyl) ethane toxicity, 255±258 Bisphenol A, estrogen mimic, 236±237 Blackbody radiation, 39±45 Black smokers, see hydrothermal vents Boiling water nuclear reactors, 613 Boltzmann factor, 74, 86 Boron biological role, 348, 399 boron neutron capture therapy, 594 drinking water standards, 426 environmental sources, 348 toxicity, 348, 399 Brachytherapy, 594±595 Breast cancer 1,1,1-dichloro-2,2-bis(pchlorophenyl)ethylene link, 237 nuclear medicine, 594±599 Breeder reactors, nuclear ®ssion power plants sodium-cooled, fast breeder reactors, 615±616 thermal breeder reactors, 616 Blemsstrahlung, 514, 525±527, 605 Bromine atoms stratosphere reactions, 112, 113 biological role, 350, 410±411 drinking water standards, 426 environmental sources, 350, 410 toxicity, 350 Bromo¯uorocarbons, structural types, 239 Buffer capacity, 310±311

C Cadmium in batteries, 745±746 biological role, 350, 390±392 drinking water standards, 426 environmental sources, 350 half-life, 566 recovery from ore, 451 in sewage sludge, 435 toxicity, 350, 391±392 Calcite, 444 Calcium abundance, 446 biological role, 349, 382±383

coordination chemistry in aqueous media, 327, 334±335 in detergents, 197 environmental sources, 349, 382 irrigation water quality, 441 ocean composition, 417±418, 420 toxicity, 349 Calcium carbonate in cements, 476±477 deposits, 382 sulfur dioxide scrubber, 374±375 Calcium hydroxide, in cements, 476±477 Calcium oxide, in cements, 476±477 Californium, in brachytherapy, 595 Cancer, see also Toxicity 1,1,1-dichloro-2,2-bis(p-chlorophenyl) ethylene link, 237 radiation therapy, 594±595, 598±599 Caprolactam, structure, 790 Carbamate, insect resistance, 274±276 Carbaryl, insect resistance, 276, 286 Carbofuran, resistance, 276 Carbon biological half-life, 550 biological role, 348 carbon cycle, 354±362, 463 decay scheme, 14 C, 512 environmental sources, 348, 355 half-life, 14 C, 512, 564±565 isotope fractionation, 584 isotopic ratios, 353±354, 568±569 radiometric age determination, 14 C, 585±592 toxicity, 348 Carbonates carbon cycle, 354±362, 463 in cements, 476±477 deposits, 382 sulfur dioxide scrubber, 374±375 Carbon dioxide atmospheric concentration, 16±18, 22, 56±57 carbon cycle, 354±362, 463 carbonic acid chemistry, 308, 311±317 global warming effects, 14, 56±59, 61 infrared radiation absorption, 45±46 isotope fractionation, 584 Kyoto Protocol, 13, 760 lake strati®cation turnover, 305 sequestration, 357±359, 385 tropospheric reactions, 132





Carbonic acid acid±base reactions, 308, 314±315 aqueous chemistry, 311±317 soil weathering, 461 Carbon monoxide air pollution reduction, 172, 175±178 atmospheric concentration, 16, 19 catalytic conversion, 175 in internal combustion engines, 173 new vehicle emission standards, 172 toxicity, 359 Carbon tetrachloride atmospheric lifetime, 239±241 structure, 239 Carbon tetra¯uoride in aluminum production, 459 lifetime, 239 Carbonyl groups octane enhancement, 179 photodecomposition role, 216 Carnot cycle, 691±692, 750 Catalytic converters, combustion emission reduction, 175±177 Catechol, salicylic acid oxidation, 205 Cements, 476±477 kilns for hazardous waste disposal, 477 Cesium biological half-life, 550 in consumer products, 601 decay scheme, 137 Cs, 508 in fallout, 137 Cs, 631±632, 653, 670±678 half-life, 137 Cs, 550, 639 Ireland radiation incident, 662±663 toxicity, 632, 653±654 CFC's, see Chloro¯uorocarbons Chapman cycle, 104 Chappuis bands, 101 Chelation coordination chemistry in aqueous media complexing applications, 333±335 complex stability and lability, 330±333 metal±ligand preferences, 327±329 heavy metal poisoning, 381 Chemical oxygen demand, biodegradable organic compounds, 206 Chernobyl, 552, 618, 667±678 Chloramines, water puri®cation, 430 Chlordane synthesis, 260±261 Chlorination of organic compounds, 225±227, 429±430 water puri®cation, 429±430

Chlorine atmospheric lifetime, 241 atoms stratosphere reactions, 109±110, 241 biological role, 349, 409±410 domestic water treatment, 426±430 environmental sources, 349 half-life, 564 ocean composition, 417±418 in paper production, 212 toxicity, 349 Chlorine dioxide, in water puri®cation, 431 Chlorine oxide, upper atmosphere reactions, 109±110, 113, 119, 121±122 Chlorobenzofurans, reactivity, 248 Chloro¯uorocarbons atmospheric lifetimes, 239±241 global warming potentials, 57±59 overview, 238±239 phaseout of use, 287±288 regulation, 122±125 structural types, 239 upper atmosphere reactions, 107±110, 113±114, 239 volcanic, 412 Chromium biological role, 349, 388±389 drinking water standards, 426 environmental sources, 349 recovery from ore, 451 in sewage sludge, 435 toxicity, 349, 389 Chrysotile, 444, 478 Cities, see Urban areas Clay aluminosilicate clays, 465±466 description, 444, 474 hydrated metal clays, 466±467 Clean Air Act, 176, 178, 182 Clean up procedures air pollution carbon monoxide, 172, 175±176, 178±180 lead, 172 nitrogen oxides, 172, 175±177, 368±369 ozone, 172, 240±241 particulates, 172, 182 sulfur dioxide, 172, 374±375 urban centers, 180±181 oil spills, 161±164 soil contamination, 469±473 water treatment, see Water systems





Climate, see also Global climate changes energy balance of the earth, 39±49 greenhouse effect, 44±47 historical perspectives, 49±53 solar radiation, 39±49, 54 microclimates, 63±65 ocean current effects, 35, 302±303 temperature inversions, 65±69 Coal conversion to hydrocarbons, Bergius process, 188±189 ferrous sul®de source, 386 formation, 182±184 gasi®cation, 184±187, 699±700 liquefaction process, 187±188 mercury source, 381 methane synthesis, 699±701 overview, 182, 697±698 radioactivity, 567 reserves, 695 structure, 182±184 Cobalt biological role, 349 in consumer products, 601 decay scheme, 60 Co, 506 environmental sources, 349 half-life, 60 Co, 506 JuaÂrez Mexico radiation incident, 661±662 recovery from ore, 451 toxicity, 349 Cold fusion, 626 Cold war nuclear waste, 648±651 nuclear weapons, 634±635 Collisional quenching, photochemical kinetics, 87 Colloids in aqueous media, 340±341 in sewage sludge, 436 Composting, waste disposal, 775±777 Comprehensive Test Ban Treaty, 630 Compton scattering, 529±531 Computed tomography, x-ray sources, 593 Computer models, climate change, 61±63 Construction materials, naturally occurring radioactivity, 581 Consumer products radiation sources, 599±601, 657 recycling

glass, 770±771, 783±784 metal, 770±771, 785±786 motor oil, 153±154 overview, 770, 783 paper, 770±771, 784 plastics, 770±771, 786±791 mixed postconsumer plastics, 788 reuse, 788±789 tertiary recycling, 789±791 Coordination chemistry, in aqueous media, 324±340 complexing applications, 333±335 lability, 330±333 in natural systems, 335±339 stability, 330±333 coordination number, 325±327 description, 324±325 geometry, 325±327 metal±ligand preferences, 327±329 water as a ligand, 329±330 Copper biological role, 350, 389±390 coordination chemistry in aqueous media, 326, 332, 335 drinking water standards, 426 environmental sources, 350, 390 recovery from ore, 451 in sewage sludge, 435 toxicity, 350, 390 Coriolis effect, 31±33 Corporate average fuel economy, 174±175 Cosmic radiation, 562±564 population dose, 657±658 quality factor, 563±564 Covalent bonds, bond energy, 298 Crocidolite, 444, 478, 480 Crude oil, see Petroleum Cryolite, 444 Cyanide drinking water standards, 427 gold recovery, 452, 454, 459±460 mining release, 460 toxicity, 359, 460 Cyclic dioxides, crude oil weathering, 160 Cytochrome P-450 detoxi®cation, 235 hydrocarbon degradation, 204±205 1,1,1-trichloro-2,2-bis(p-chlorophenyl) ethane degradation, 254





 Dacron, synthesis, 212 Dating methods, radiometry, 585±592 DDE, see 1,1-Dichloro-2,2-bis (p-chlorophenyl)ethylene DDT, see 1,1,1-Trichloro-2,2-bis (p-chlorophenyl)ethane Detergents overview, 194, 197±198 surfactants biological oxygen demand, 206 linear alkylsulfonate synthesis, 198±200 microbial metabolism, 201±206 nonionic alcohol ethoxylate synthesis, 200±201 Deuterium abundance, 624 nuclear fusion, 516±517 thermonuclear power plants, 624±626 Dialkyl phosphorochloridate, synthesis, 271 Diatomic molecules, spectroscopic state designations, 796±799 1,1-Dichloro-2,2-bis(p-chlorophenyl)ethylene environmental degradation, 253±254 hormonal activity, 237 insect resistance, 274±276 Dichlorodiphenyltrichloromethane, see 1,1, 1-Trichloro-2,2- bis(p-chlorophenyl) ethane Dichloromethane, hydrolytic degradation, 234 2,4-Dichlorophenoxyacetic acid environmental degradation, 266±270 overview, 265 synthesis, 265±266 toxicity, 267±270 Dieldrin environmental degradation, 263±264 insect resistance, 276 synthesis, 260±261 Diels-Alder reaction, polychlorinated cyclodiene synthesis, 260±262 Diesel engines, pollution reduction, 182 Di(2±ethylhexyl)phthalate, health concerns, 207±208, 210 Dipole±dipole bonds bond energy, 298 solubility effects, 304 Displacement reactions organochlorine compounds, 227±228 Distillation, water puri®cation, 437 Distrophic lake, 300

Disulfoton, resistance, 276 DNA, ionizing radiation effects, 535±537 Dolomite, 444 Drinking water, see Water systems

 Earth, age, 586 a-Ecdysone, insect control, 282 Einstein energy equation, 489±490 Einstein relationship, 76 Electric and magnetic ®elds health effects, 78±80 Electrodialysis, water puri®cation, 437±438 Electrolysis, hydrogen production, 742±743 Electromagnetic radiation, see also speci®c types photochemistry, 75±83 light absorption, 77±83 light properties, 75±77 Electron capture energetics, 513±514 El NinÄo/Southern Oscillation, 53, 116 EMF's, see Electric and magnetic ®elds Endrin, resistance, 276, 286 Energy electricity generation from fuels, 750±754 fossil fuels, see Fossil fuels future prospects, 754±761 United States energy production, 754±756 world energy production, 756±761 geothermal energy, 728±730, 738 nuclear ®ssion, 520±521 thermonuclear, 516±517 overview, 7, 687±689, 761 solar energy, see Solar energy storage, 737±750 batteries, 744±750 description, 737±740 ¯ywheels, 740±741 hydrogen, 741±744 pumped storage, 740 superconductivity, 741 thermodynamics, 689±694 laws of thermodynamics, 689±693 units of energy and power, 694 water energy, 733±737 hydroelectric power, 733±734, 739±740 tidal power, 734±735, 739 wave power, 735±737, 739 wind energy, see Wind Energy balance, climate effects, 39±49 greenhouse effect, 44±47





Energy balance, climate effects, (continued) historical perspectives, 49±53 solar radiation, 39±49, 53±54 Entisols, 467 Environmental hormones, toxicity, 235±238 Environmental Protection Agency arsenic standards, 406 oil combustion emission standards, 154, 156 pesticide bans, 264, 271 radon limits, 572±573, 648 Essential elements for life, 353 Estradiol structure, 256 1,1,1-trichloro-2,2-bis(p-chlorophenyl) ethane toxicity, 256 Estrogen bio¯avonoids, 238 haloorganic compound effects, 235±237 Ethanol characteristics, 178 octane enhancement, 178±179 Ethoxylates degradation, 203±205 synthesis, 200±201 Ethylene, surfactant synthesis, 194 Ethylenediamine, chelation in aqueous media, 327 Ethylenediaminetetraacetic acid chelation in aqueous media, 90, 334±335 in nuclear medicine, 596 Eutrophication, 301 Eutrophic lake, 300

 Fallout from nuclear accidents, 664±665, 670±678, 679 from nuclear weapons, 631±632 human internal exposure, 653±655 Fats, surfactant synthesis, 194 Fatty acids, surfactant synthesis, 194, 201±202 Feldspar, 445 Fenvalerate, insect resistance, 276 Ferrous sul®de, environmental sources, 386 Fertilizer, potassium, 378±379 Fertilizers global use, 378±379 nitrogen, 366±370, 378±379 phosphorus, 375±379 sewage sludge, 434

Fischer±Tropsch process, coal liquefaction, 187±188 Fish crude oil effects on marine life, 165 mercury accumulation in, 397±399 plastic refuse effects, 213±214 polychlorinated biphenyl toxicity, 246 Fission, see Nuclear ®ssion Fission track counting, age determination, 587 Flocculating agents, domestic water treatment, 427±429 Fluidized-bed reactor, plastic waste pyrolysis, 790±791 Fluorescence, photochemical kinetics, 87±88 Fluoride, drinking water standards, 427 Fluorinated ethers CFC replacements, 124 lifetimes, 114 ozone depletion potentials, 114 Fluorine biological role, 348, 411 environmental sources, 348, 411±412, 459 ozone destruction, 411 phosphate fertilizer reactions, 377 toxicity, 348 water ¯uoridation, 411 Fluorocarbons, see also Chloro¯uorocarbons from aluminum production, 459 Flywheels, energy storage, 740±741 Food fallout contamination, see Fallout irradiation, 603±606 dose of ionizing radiation, 604±607 naturally occurring radioactivity, 580±581 radura, symbol for irradiated food, 606 Food and Agriculture Organization, 603±606 Food and Drug Administration, 605 Formaldehyde formation, dichloromethane degradation, 234 tropospheric reactions, 133±134, 141 Formyl radical, tropospheric reactions, 134, 138 Fossil fuels coal, see Coal liquid hydrocarbon fuels, 696±697 oil shales, 696±697 petroleum, see Petroleum synthetic products, 697 tar sands, 696±697 natural gas, 698 overview, 694±696





Friedel±Crafts reaction surfactant synthesis, 200 1,1,1-trichloro-2,2-bis (p-chlorophenyl)ethane synthesis, 252 Fuel cells, 750±754 Fulvie acid, 335±336 Fusion, see Cold fusion; Nuclear fusion

 Gamma radiation cosmic radiation, 562±564 decay energetics, 505±508 dose rate estimation, 546 exposure rate estimation, 544±545, 657 health effects acute deterministic effects, 547±548 average annual dose, 657±659 external sources, 547±549, 655, 657 internal sources, 549±550, 555±559 ionizing radiation, 537±538 stochastic effects, 537±538, 548±549 interactions, 529±533 Compton scattering, 529±531 energy absorption, 530±533 pair production, 530 photoelectric effect, 529 total attenuation, 530±533 properties, 77±78 Gas-cooled, graphite-moderated nuclear reactors, 614±615 Gases, see speci®c gases Gasoline, see Petroleum Geothermal energy costs, 738 description, 728±730 Glass description, 475 recycling, 770±771, 783±784 Global Ozone Observing System, 115 Global climate changes causes, 53±63 albedo changes, 47±48, 59±61 computer models, 61±63 greenhouse effect changes, 56±59 Milankovitch theory of orbital variation, 55±56 volcanic activity, 59±61 El NinÄo/Southern Oscillation, 53, 116 energy balance of the earth, 39±49 greenhouse effect, 44±47 historical perspectives, 49±53

solar radiation, 39±49, 54 global warming potentials, 57±59 Intergovernmental Panel on Climate Change, 13, 355±356 overview, 3±4, 14 temperature rise, 13±14 Gold, recovery from ore, 452, 459±460 Granite, 445 Greenhouse effect, see also Global climate changes through history, 56±59 energy balance of the earth, 44±47 Grotthus±Draper law, 77 Groundwater, water cycle, 296±297 Gypsum, in cements, 476±477

 Hadley cells, 30±31, 33 Half-life biological, 550 chemical reaction, 85 effective, 549±550 ®ssion products, 638±639 kinetics, 85 radioactive decay, 495±497, 550, 564±566, 639 Halogens, 409±412 Haloorganic compounds chloro¯uorocarbons, see Chloro¯uorocarbons 2,4-dichlorophenoxyacetic acid, see 2, 4- Dichlorophenoxyacetic acid environmental degradation, 224±225 environmental hormones, 235±238 hydro¯uorocarbons, see Hydro¯uorocarbons lindane, see Lindane microbial degradation, 225, 231±234 hydrolytic degradation, 234 oxidative degradation, 233±234 reductive degradation, 232±233 organochlorine compound chemistry, 225±231 reactions, 227±231 displacement reactions, 227±228 elimination reactions, 228 environmental reaction pathways, 228±231 synthesis, 225±227 organophosphorus insecticides, see Organophosphorus insecticides overview, 223±224, 244±245 perhalogenated organics





Haloorganic compounds (continued) atmospheric lifetimes, 239±241 overview, 238±239 structural types, 239 phaseout of use, 287±288 polybrominated biphenyls, see Polybrominated biphenyls polychlorinated biphenyls, see Polychlorinated biphenyls polychlorinated cyclodienes, see Polychlorinated cyclodienes toxicity, 234±238 Hard±soft scale, metal±ligand interactions, 328±329, 333 Hard water, properties, 316 Hartley continuum, 101 Hazardous waste, incineration, 477, 780±781 Hematite, 445 Hemoglobin methemoglobinemia, 364 structure, 338 Henry's law, gas solubilities, 304±305, 312, 322, 421 Heptachlor environmental degradation, 263±264 synthesis, 260±261 Herbicides, see speci®c herbicides Herzberg continuum, 95 Hexachlorocyclopentadiene, synthesis, 260±262 1,2,3,4,5,6±Hexachlorocyxlohexane environmental degradation, 260 synthesis, 258±259 High density polyethylene, recycling, 787±788 Histosols, 467 Hormones, see also speci®c hormone environmental hormones, 235±238 insect control, 281±283 Humic acid, 335±336 Hybrid vehicles, 182 Hydrocarbons coal, see Coal internal combustion engines, 168±170 microbial metabolism, 201±206 overview, 147±148 petroleum, see Petroleum sources atmospheric pollution, 170±181 automobiles, 171±175 catalytic converter effects, 175±177 gasoline additives, 177±179

marine pollution, 150±158 catastrophic oil spills, 155±158 description, 150±151 natural sources, 151±152 off shore wells, 152 transportation, 154±155 waste runoff, 153±154 urban center pollution, 179±182 low-emission automobiles, 181±182 reduction plans, 180±181 Hydrochloric acid acid±base reactions, 308 upper atmosphere reactions, 111±112 Hydrochloro¯uorocarbons, see also Chloro¯uorocarbons atmospheric lifetimes, 242±243 ozone depletion potential, 114 global warming potentials, 58±59 phaseout of use, 287±288 regulation, 123±124 structural types, 239 Hydroelectric power costs, 739 description, 733±734 pumped storage, 740 Hydro¯uorocarbons atmospheric lifetimes, 114, 123, 242±243 overview, 238±239 ozone depletion potential, 114 structural types, 239 Hydrogen abundance, 446 atmospheric concentration, 16 biological half-life, 550 biological role, 348 energy storage, 741±744 environmental sources, 348 fuel cells, 742±743, 750±754 half-life, 3 H, 550, 564±565, 639 production, direct solar energy conversion, 727±728 toxicity, 348 Hydrogen bonds bond energy, 298 solubility effects, 304 water chemistry, 298±299 Hydrogen sul®de radicals, tropospheric reactions, 139±140 Hydrolysis chlorine, 409 haloorganic compound degradation, 224, 234





polymer degradation, 216±217 water as a ligand, 329±330 Hydroperoxides, crude oil weathering, 160 Hydrothermal vents, 449±450 Hydroxyl radical crude oil weathering, 160 radiolysis of water, 535±537 tropospheric reactions, 131±134, 137±140 a-Hydroxy radical, tropospheric reactions, 138 Hypolimnion, 300

 Ice density, 299, 302±303 isotope fractionation, 584 melting effects, 303 Igneous rock, 445 Implant therapy, radiation sources, 594±595, 653 Inceptisols, 467 Incineration, waste disposal, 477, 777±781 Infrared radiation atmospheric absorption, 44±47 properties, 77±78 solar emission, 42±46 Inipol EAP 22, oil spill clean up, 163 Insecticides, see also speci®c insecticides biochemical insect control, 276±285 attractants, 280±281 bacteria, 283±285 hormones, 281±283 pheromones, 277±280 viruses, 283 food irradiation, 603±606 integrated pest management, 285±287 organophosphates environmental degradation, 273±274 overview, 270±271 resistance, 274±276, 286 synthesis, 271±272 toxicity, 273 polychlorinated cyclodienes, 260±264 resistance, 274±276, 286 Integrated pest management, 285±287 Internal combustion engines, hydrocarbon emissions, 168±170 Internal conversion, radioactive decay energetics, 507 International Atomic Energy Agency, 636 International Commission on Radiological Protection, 541

International Energy Outlook 2000, 756±761 International Thermonuclear Experimental Reactor, 625 Invertebrates crude oil effects on marine life, 165 Iodine biological half-life 550 biological role, 351, 410±411 in brachytherapy, 125 I, 594 decay scheme, 131 I, 507 environmental sources, 351, 410 in fallout, 632, 653, 672±678 half-life 129 I, 564±565, 639 131 I, 507, 632, 676 in nuclear medicine, 598 toxicity, 351, 632, 653 transmutation, 129 I, 645 Ion exchange, water puri®cation, 438 Ionizing radiation biological effects, 535±537 charged particle interactions, 522±528 alpha particles, 523±524 description, 522±523 negatrons, 524±528 positrons, 524±528 dose average annual dose, U.S. population, 657±659 dose±effect correlation, 550±553 high-level dose, 550±552 low-level dose, 552±553 estimation, 546±547 alpha radiation, 547 beta radiation, 546±547 gamma radiation, 546 external exposure, 547±549, 655 internal exposure, 655±657 natural human tissue radioactivity, 655±656 quality factor, 540±541 regulatory limits in U.S., 659±661 units, 539±544 weighting factors, 540±543 worker safety, 619 exposure gamma radiation, 544±545 health effects, 537±538 internal exposure pathways, 651±655 rate estimation, 544±545





Ionizing radiation (continued) units of measure, 538±539 neutron interactions, 533±534 nuclear accidents, see Nuclear accidents source applications, 589±606 focused-beam sources, 593±594 food irradiation, 603±606 implant therapy, 594±595 multifarious sources, 599±606 neutron activation analysis, 602±603 nuclear medicine sources, 595±599 symbol, 661 thermal neutron analysis, 602±603 treatment of pollutants, 602 X and gamma ray interactions, 529±533 Compton scattering, 529±531 energy absorption, 530±533 pair production, 530 photoelectric effect, 529 total attenuation, 530±533 Ireland, radiation incident, 662±663 Iron abundance, 446 biological role, 349, 364, 383±388 carbon dioxide control, 385 coordination chemistry in aqueous media, 328, 332, 335±339, 383±384 drinking water standards, 426 environmental sources, 349, 386±387 ocean composition, 417±418 recovery from ore, 452, 457±458 recycling, 770±771 soil contamination clean up, 472 toxicity, 349, 388 Irrigation, water quality, 440±441 Isotope dilution, 586 Isotope fractionation applications, 582±584, 590±592 dependence on isotopic mass, 488 Isotopic ratios, overview, 353±354 Itai-Itai disease, 392

J Joint European Torus, thermonuclear power, 625 Juvenile hormone, insect control, 281±283

K Kaolinite, 445, 462, 465 Kepone, toxicity, 236±237 Kinetics

photochemical processes, 87±89 production of radionuclides, 502±504 radioactive decay, 494±502 thermal processes, 83±87 Kraft process, paper production, 212 Kyoto Protocol, 13, 759±760

L Lambert's law, 80±82 Land®lls, waste disposal, 5, 772±775 Latex, biodegradation, 207 Lead air pollution reduction, 172 in batteries, 745 biological role, 351, 400±405 drinking water standards, 426 environmental sources, 351, 402±405 in gasoline, 169±170, 177±179, 401 pigments, 402±403 recovery from ore, 452 in plumbing, 403±404 in sewage sludge, 435 toxicity, 351, 401, 404±405 Ligands, coordination chemistry of aqueous media metal±ligand preferences, 327±329 water as a ligand, 329±330 Limestone, 445 Lindane environmental degradation, 260 synthesis, 258±259 Linear alkylsulfonates degradation, 203±205 synthesis, 198±200 Linear energy transfer cosmic radiation, 563±564 de®nition, 534 ionizing radiation, 534±535, 539±541 values, 534, 540 Linear polyatomic molecules, spectroscopic state designations, 799±800 Liquid metal fuel reactors, 617 Lithium in batteries, 746±748 biological role, 348 environmental sources, 348 nuclear reactor coolant, 626 toxicity, 348 Lurgi process, coal gasi®cation, 185±186, 699±700





M Magnesium abundance, 446 biological role, 348, 382±383 coordination chemistry in aqueous media, 327, 339 in detergents, 197 environmental sources, 348, 382 irrigation water quality, 441 ocean composition, 417±418, 420 toxicity, 348 Magnesium oxide, sulfur dioxide scrubber, 374 Magnetic resonance imaging, (MRI), 593±594, 597 Magnetite, 445 Malathion, synthesis, 272 Mammals crude oil effects on marine mammals, 166 plastic refuse effects, 213±214 toxic chemicals, see Toxicity Manganese abundance, 446 biological role, 349, 389 drinking water standards, 426 environmental sources, 349, 389 recovery from ore, 452 toxicity, 349, 389 Marble, 445 Marine environments crude oil effects on marine life, 164±168 birds, 165±166 ®sh, 165 invertebrates, 165 marine mammals, 166 sea turtles, 167±168 pollution sources catastrophic oil spills, 155±158 natural sources, 151±152 off shore wells, 152 overview, 150±151 plastics, 213±214 transportation, 154±155 waste runoff, 153±154 Mercury biological role, 351, 390±399 coordination chemistry in aqueous media, 326, 328 drinking water standards, 426 environmental sources, 351, 381, 393±396 mercury cycle, 397 recovery from ore, 452

in sewage sludge, 435 toxicity, 351, 392, 394, 396, 398±399 Metals, see also speci®c metals biological importance, 379±381 coordination chemistry of aqueous media, 324±340 complexing applications, 333±335 lability, 330±333 in natural systems, 335±339 stability, 330±333 coordination number, 325±327 description, 324±325 geometry, 325±327 metal±ligand preferences, 327±329 metal oxide adsorption, 342±343 water as a ligand, 329±330 recovery from ores, see Ore, metal recovery from recycling, 770±771, 785±786 in sewage sludge, 434±435 Metamorphic rock, 445 Methane anaerobic digestion of biological wastes, 777 atmospheric concentration, 16, 20, 56±58 combustion energetics, 490 global warming potentials, 58±59, 361±362 infrared radiation absorption, 46 in natural anaerobic water systems, 440 natural gas, 698 natural sources, 360, 698 properties, 360±361 synthesis from coal, 699±701 tropospheric reactions, 132±133 Methane hydrate, properties, 360±361 Methoxychlor analogues, 255 environmental degradation, 254 overview, 252±253 synthesis, 252 toxicity, 253 Methyl bromide atmospheric lifetime, 241 overview, 243±244 Methyl chloride atmospheric lifetime, 241 overview, 243±244 Methylchloroform atmospheric lifetime, 240±241 structure, 239





Methylcyclopentadienylmanganese tricarbonyl, octane enhancement, 179 Methyl mercury properties, 396±398 toxicity, 396±398 Methyl parathion, synthesis, 272 Methyl tert-butyl ether, in gasoline, 178±179 Mica, 445 Microbial degradation detergents, 201±206 haloorganic compounds, 225, 231±234 hydrolytic degradation, 234 oxidative degradation, 233±234 reductive degradation, 232±233 hydrocarbons, 201±206 napthalene, 205 polychlorinated biphenyls, 249±251 aerobic biodegradation, 249±250 anaerobic biodegradation, 250±251 sewage sludge, 435 soaps, 201±206 surfactants, 201±206 Microclimates, 63±65 Microcline, 445 Microwaves properties, 77±78 solar emission, 43 Milankovitch theory, orbital variation, 55±56, 591 Minamata, 398 Minerals, composition, 443±448 Mining, see Ore, metal recovery from Mirex environmental degradation, 264 synthesis, 260±262 Mollisols, 467 Molten salt nuclear reactors, 617 Molybdenum biological role, 350, 364 drinking water standards, 427 environmental sources, 350 recovery from ore, 452 toxicity, 350 Monazite, thorium source, 567±568 Monocrotophos, resistance, 276 Montmorillonite, 445, 465±466 Montreal Protocol, 13, 122±123, 125, 240±241 Motor oil, see also Petroleum recycling, 153±154

 Napthalene, microbial oxidation, 205 National Appliance Energy Conservation Act, 756 National Ignition Facility, 625 National Toxicology Program, 207, 268 Natural gas description, 698 radon content, 577 reserves, 695 synthesis from coal, 699 Negatrons interactions with matter, 524±528 radioactive decay energetics, 508±511 Neon, atmospheric concentration, 16 Neutrons activation analysis, 602±603 boron neutron capture therapy, 594 ionizing radiation interaction with matter, 533±534 moderation, 533 production non®ssion reactions, 521 nuclear ®ssion, 517±521 as source of ionizing radiation, 533±534 Nickel in batteries, 745±746 biological role, 350 coordination chemistry in aqueous media, 332, 335 drinking water standards, 427 environmental sources, 350 recovery from ore, 453 in sewage sludge, 435 toxicity, 350, 379±380 Nitrate drinking water standards, 427 in natural anaerobic water systems, 439 in sewage sludge, 436±437 Nitrate radical, tropospheric reactions, 134±135, 141 Nitric acid, upper atmosphere reactions, 119±120 Nitrilotriacetic acid, phosphate replacement in detergents, 334 Nitrite drinking water standards, 427 nitrosamine formation, 364 Nitrogen atmospheric concentration, 16, 23 biological role, 348, 363±364





environmental sources, 348, 365 in fertilizers, 366±367, 378±379 ®xation, 362±367 nitrogen cycle, 362±365, 369 petroleum combustion, 150 photochemistry troposphere reactions, 129±135 upper atmosphere reactions, 93±95 properties, 362±370 toxicity, 348 Nitrogen oxides absorption spectrum, 130 air pollution reduction, 172, 175±177, 367±369 aqueous redox chemistry, 362 catalytic conversion, 175±177 equilibrium pressures, 368 global warming potentials, 58±59 in internal combustion engines, 173, 367 new vehicle emission standards, 172 petroleum combustion, 150 properties, 362±370 tropospheric reactions, 127±129, 135±140 upper atmosphere reactions, 94±95, 106±107 Nitrosamines, 364 Nitrous oxide, isotope fractionation, 584 Norrish processes, polymer photodecomposition, 216 Nuclear accidents, 661±680 Chernobyl, 552, 618, 667±678 gauging sources, 662 nuclear fuel processing plants, 679±680 nuclear reactors, 663±678 radioactive waste, 678±679 therapy sources, 661±663 Three Mile Island, 665±667, 706 Windscale, 663±665 Nuclear ®ssion natural reactors, Oklo phenomenon, 623±624 neutron induced, 517±521 power plants, see Nuclear power plants Nuclear fusion cold fusion, 626 reactions, 516±517 thermonuclear power plants, 624±626 Nuclear magnetic resonance spectroscopy description, 489 radiation sources, 593 Nuclear medicine

average annual exposure, 657±659 radiation sources, 595±599 Nuclear Non-Proliferation Treaty, 632±634 Nuclear power plants countries with plants, 703±704 ef¯uents, 620±622 environmental concerns, 701 factors affecting choice of use, 705±709 alternative energy availability, 705±706 costs, 707±709 fuel, 707 safety, 706±707 spent fuel, 707 future directions, 622±623 nuclear fuel, 607±611, 615, 635, 637±641 reactor types, 607±608 safety features, 617±619 reactor safety, 617±619 worker doses, 619 status United States, 704±705 worldwide, 701±704 types, 611±617 boiling water reactors, 613 gas-cooled, graphite-moderated reactors, 614±615 liquid metal fuel reactors, 617 molten salt reactors, 617 organic-cooled reactors, 617 pressurized water reactors, 611±613 sodium-cooled, fast breeder reactors, 615±616 thermal breeders, 616 water-cooled, graphite-moderated reactors, 613±614 Nuclear radiation, see Radioactivity Nuclear reactions energetics, 489±494 induced reactions charged-particle reactions, 516±517 kinetics, 502±504 non®ssion neutron production, 521 nuclear ®ssion, 517±521 nuclear fusion, 516±517 photonuclear reactions, 517 kinetics, 494±504 induced nuclear reactions, 502±504 radioactive decay, 494±502 Nuclear Regulatory Commission, 543, 622, 648, 701, 707





Nuclear waste cold war mortgage, 648±651 disposal methods, 637±648 ef¯uents, 620±622 high-level waste, 637±645 low-level waste, 647±648 mill tailings, 636, 648±649 spent nuclear fuel, 637±645 transuranic waste, 646±647 nuclear accidents, 678±679 types, summary of, 635±636 Nuclear weapons, 627±635 cold war heritage, 634±635 fallout and rainout, 631±632 production, 627±630 proliferation, 632±634 testing, 630±631 types, 627 Nuclear winter, 61 Nuclide, de®nition, 484 Nylon, structure, 208, 709

O Oak Ridge Nuclear Facility, 643, 649 Oceans composition, 415±417 currents, 301±302 energy resource ocean thermal energy conversion, 719±720, 738 tidal power, 734±735, 739 wave power, 735±737 incineration ships, 780 model system, 417±421 radioactive waste dumping, 642 thermal vents, 449±450 Ocean thermal energy conversion, 719±720, 738 Octane enhancement, 177±179 in internal combustion engines, 168±170 ODP, see Ozone depletion potential Oil, see Fats; Petroleum Oil shales, petroleum production, 696±697 Oil spills crude oil effects on marine life, 164±168 birds, 165±166 ®sh, 165 invertebrates, 165 marine mammals, 166 sea turtles, 167±168 fate, 158±163

clean up, 161±164 weathering, 160±161 sources, 150±158 catastrophic oil spills, 155±158 description, 150±151 natural sources, 151±152 off shore wells, 152 transportation, 154±155 waste runoff, 153±154 Oklo phenomenon, natural ®ssion reactors, 623±624 Ole®ns Diels-Alder reaction, 260±262 synthesis, 194, 199±200, 228 Olivine, 445 Ore, metal recovery from, 449±460 aluminum, 451, 458±459 bacterial mining, 456 gold, 452, 454, 459±460 iron, 457±458 sources, 449±454 treatments, 454±456 concentration, 454±455 puri®cation, 455±456 reduction, 455 re®ning, 455±456 roasting, 455 Organic-cooled nuclear reactors, 617 Organochlorine compounds, 225±231, 409±410 reactions, 227±231 displacement reactions, 227±228 elimination reactions, 228 environmental reaction pathways, 228±231 soil contamination, 472 synthesis, 225±227 Organophosphorus insecticides environmental degradation, 273±274 overview, 270±271 resistance, 274±276, 286 synthesis, 271±272 toxicity, 273 Orlon, synthesis, 210±211 Orthoclase, 445 Otto cycle, 690±691 Oxamyl, resistance, 276 Oxidation haloorganic compound degradation, 224±225 napthalene degradation, 205





polymer degradation, 215±216 Oxidation±reduction processes, aqueous media, 320±324 Oxisols, 467±468 Oxygen abundance, 446±447 atmospheric concentration, 16, 23±24 biological role, 348 environmental sources, 348 isotope fractionation, 583±584 toxicity, 348 upper atmosphere reactions, 95±100 Oxygenates, in gasoline, 178 Ozone air pollution reduction, 172, 240±241 isotope fractionation, 584 Montreal Protocol, 13, 125, 240±241 overview, 3±4 photochemistry tropospheric reactions, 130±131, 134, 136, 141 upper atmosphere reactions, 100±125 Antarctic ozone hole, 117±121, 241 Arctic ozone hole, 121±122 catalytic destruction in the stratosphere, 105±117, 247±248 clean stratosphere, 100±105 ozone-depleting substance control, 113±114, 122±125 radiation absorption, 29±30, 45±46, 102±104 stratospheric chlorine correlation, 241 Ozone depletion potential, 113, 114 Ozonolysis, domestic water treatment, 431

P PAN, see Peroxyacl nitrate Paper overview, 212 recycling, 770±771, 784 n-Paraf®ns, surfactant synthesis, 194 Parathion environmental degradation, 273±274 synthesis, 272 Partial freezing, water puri®cation, 438 Particulates air pollution reduction, 172, 182 atmospheric composition, 24±26 PCB's, see Polychlorinated biphenyls Pentachlorophenol, degradation, 233 Per¯uorocarbons, 469 Permethrin, resistance, 276

Peroxides, formation in polymer degradation, 215±216 Peroxyacyl nitrate, tropospheric reactions, 136, 139, 141±142 Peroxyacyl radicals, tropospheric reactions, 139 Persistent organic pollutants, see also speci®c compounds environmental hormone, 238 Pesticides, see speci®c pesticides Petroleum characteristics, 148±150 crude oil effects on marine life, 164±168 birds, 165±166 ®sh, 165 invertebrates, 165 marine mammals, 166 sea turtles, 167±168 internal combustion engines, 168±170 marine pollution, 150±158 catastrophic oil spills, 155±158 description, 150±151 natural sources, 151±152 off shore wells, 152 transportation, 154±155 waste runoff, 153±154 oil spill fate, 158±163 clean up, 161±164 weathering, 160±161 overview, 147±148, 696 production from coal, 697 from tar sands, 696±697 reserves, 694±695 surfactant use, see Surfactants pH acid±base reactions, 310±311, 317±319 acid rain, see Acid rain carbonic acid chemistry, 308, 311±317 irrigation water quality, 441 model ocean systems, 417±418, 421 solubility relationship, 317±319 Phenol ethoxylates degradation, 203±205 synthesis, 200±201 Pheromones, biochemical insect control, 277±280 Phorate, resistance, 276 Phosmet, resistance, 276 Phosphates coordination chemistry in aqueous media, 334





Phosphates (continued) in detergents, 194, 197±198 in fertilizers, 375±379 microbial metabolism, 201±206 in sewage sludge, 436 Phosphorescence, photochemical kinetics, 87 Phosphoric acid derivatives, synthesis, 271 Phosphorus abundance, 446 biological role, 349, 377 environmental sources, 349 half-life, 32 P, 564 properties, 375±379 toxicity, 349 Photochemistry atmospheric reactions, 91±145 overview, 91±93 troposphere reactions, 126±142 nitrogen oxides, 127±129, 135±140 smog characteristics, 3, 126±129, 140± 142 urban atmospheres containing volatile organic compounds, 127±129, 135±140 upper atmosphere reactions, 93±126 nitrogen, 93±95 oxygen, 95±100 ozone, 100±125, 247±248 water, 125±126 electromagnetic radiation, 75±83 light absorption, 77±83 light properties, 75±77 haloorganic compound degradation, 224 kinetics photochemical processes, 87±89 thermal processes, 83±87 overview, 73±75 polymer degradation, 215±216 Photonuclear reactions, 517, 521 Photosynthesis, isotope fractionation, 584 Photovoltaics costs, 738 solar energy utilization, 721±727 Phthalic acid plasticizer, structure, 210 Plagioclase, 445 Planck's blackbody equation, 40 Plastics environmental degradation biodegradation, 214, 217±218 hydrolysis, 216±217 nonbiodegradable polymers, 214±215 photodecomposition, 216

photooxidation, 215±216 fate after use, 213±214 overview, 193, 207±210, 218±219 recycling, 770±771, 786±791 synthesis, 210±212 Platinum, coordination chemistry in aqueous media, 326, 328 Plutonium biological role, 352 chemical behavior in environment, 654 environmental sources, 352 in fallout, 671 half-life biological, 550 radioactive decay 238 Pu, 600, 639 239 Pu, 518, 639 nuclear ®ssion reactor fuel, 521, 608±609 in nuclear weapons, 627, 634±635 in spent nuclear fuel, 638 in thermoelectric generators and heaters, 600±601 toxicity, 352, 629 in TRU waste, 646 Podzolization, soil leaching, 468 Polar stratospheric clouds, 118±121 Pollution, see also speci®c pollutants air pollution Clean Air Act, 176, 178, 182 clean up procedures carbon monoxide, 172, 175±178 lead, 172 nitrogen oxides, 172, 175±177, 369 ozone, 172, 240±241 particulates, 172, 182 sulfur dioxide, 172, 374±375 urban centers, 180±181 hydrocarbon sources, 170±181 automobiles, 168±175 catalytic converter effects, 175±177 gasoline additives, 177±179 smog photochemistry characteristics, 3, 126±129, 140±142 nitrogen oxides, 127±129, 135±140 urban atmospheres, 129, 135±140 temperature inversion effects, 65±69 urban centers, 179±182 low-emission automobiles, 181±182 reduction plans, 180±181 de®nition, 3





environmental effects, 2±4 soil contamination, 469±473 thermal pollution, 693 water pollution crude oil effects on marine life, 164±168 birds, 165±166 ®sh, 165 invertebrates, 165 marine mammals, 166 sea turtles, 167±168 pollution sources, 150±158 catastrophic oil spills, 155±158 description, 150±151 natural sources, 151±152 off shore wells, 152 transportation, 154±155 waste runoff, 153±154 radionuclides, 578±580 Polonium biological half-life, 550 in consumer products, 600, 652 in food, 580 half-life, 210 Po, 500, 580 Polonium, in consumer products, 600, 652 Polyamides, hydrolysis, 216±217 Polyatomic molecules, spectroscopic state designations, 799±800 Poly(b-hydroxybutyrate) biodegradation, 217±218 structure, 209 Poly(b-hydroxyvalerate) biodegradation, 217±218 structure, 209 Polybrominated biphenyls overview, 244±245 toxicity, 247 Polycaprolactone, structure, 209 Polychlorinated biphenyls environmental problems, 245 microbial degradation, 249±251 aerobic biodegradation, 249±250 anaerobic biodegradation, 250±251 overview, 244±245 reactivity, 247±249 synthesis, 247±249 toxicity, 236±237, 245±247, 255±256 Polychlorinated cyclodienes environmental degradation, 262±264 insect resistance, 274±276 synthesis, 260±262 Poly(cis-1,4-isoprene), structure, 209

Polyesters hydrolysis, 216±217 structure, 209 Polyethylene biodegradation, 218 photodecomposition, 216 recycling, 787±788 structure, 208 Polyethylene glycols, biodegradation, 217 Polyethylene terephthalate biodegradation, 217 recycling, 787±789 structure, 208 synthesis, 212 Polyglycolate, structure, 209 Polyhydroxy compounds, coordination chemistry, 336 Polylactate, structure, 209 Polymers, see also speci®c types environmental degradation biodegradation, 214, 217±218 hydrolysis, 216±217 nonbiodegradable polymers, 214±215 photodecomposition, 216 photooxidation, 215±216 fate after use, 213±214 overview, 193±194, 207±210, 218±219 paper, 212 synthesis, 210±212 Poly(methyl methacrylate), structure, 208 Polyphosphates, 333, 375±376 Polypropylene photodecomposition, 216 recycling, 787±788 structure, 208 Polystyrene recycling, 787 structure, 208 Polyurethanes chemical decomposition, 789±790 hydrolysis, 216±217 structure, 209, 790 Polyvinyl acetate, structure, 209 Polyvinyl alcohol, structure, 209 Polyvinyl chloride recycling, 787±788 structure, 208 Population growth, 7±10 Porphin ring, structure, 337±338 Porphyrins, coordination chemistry, 337±339





Positron emission tomography, radiation sources, 597 Potassium abundance, 446 biological role, 349 coordination chemistry in aqueous media, 339 environmental sources, 349, 657 fertilizer, 378±379 iodide, blocking agent, 653, 667, 672 ocean composition, 417±418, 420 ocean radioactivity, 580 radiopotassium, 40 K contribution to average annual dose of ionizing radiation, 657 decay scheme, 514 environmental sources, 349, 565±566, 580±581, 652 half-life, 514, 566, 652 radiometric age determination, 587, 590 toxicity, 349 Pourbaix diagrams iron systems, 387 sulfur systems, 323 Power, units of measure, 694 Precocenes, insect control, 282±283 Pressure, equilibrium effects in aqueous media, 319±320 Pressurized water nuclear reactors, 611±613 PSC's, see Polar stratospheric clouds Pyrethroid, resistance, 274±276 Pyrite description, 445 ferrous sul®de source, 386 Pyroxene, 445

Q Quality factor, see Ionizing radiation, dose Quantum numbers, spectroscopic state designations atoms, 793±796 diatomic molecules, 796±799 overview, 793 polyatomic molecules, 799±800 Quantum yield, photochemical kinetics, 87±88 Quartz, 445 Quinolines, petroleum combustion, 150 Q value nuclear reaction energetics, 490±493, 520±521

R Radiation, see speci®c types Radiation hormesis, 553 Radiation pressure, 75 Radiation therapy, radiation sources, 594±595 Radioactivity, see also Ionizing radiation, Nuclear accidents, and Nuclear waste energetics, 504±516 kinetics, 494±504 naturally occurring distribution, 565±581 construction materials, 581 food, 580±581 outdoor air, 568±570 radon in indoor air, 570±578 rocks and soils, 565±567 thorium ores, 567±568 uranium ores, 567±568 water, 578±580 sources, 564±565 study applications, 582±592 isotope fractionation, 488, 583±584 radiometric age determination, 585±589 types of applications, 582±583 types alpha emission, 514±515 beta decay, 508±514 electron capture, 513±514 gamma-ray emission, 505±508 internal conversion, 507 isomeric transition, 505±508 negatron emission, 508±511 positron emission, 511±513 spontaneous ®ssion, 515±516 units, 494±495 Radiocarbon dating methods, 587±589 Radioisotope thermoelectric generators, 600±601 Radiopharmaceuticals, 595±599 Radio waves, properties, 77±78 Radium, 226 Ra, biological half-life, 550 in coal, 567 in consumer products, 599 in food, 580 half-life, 500 in reference man, 655 in water, 578 Radon atmospheric levels, 570





biological role, 351 in buildings, 571±578 decay scheme, 570 distribution, 573±576 environmental sources, 351, 570±573 exposure, 570±571, 656±657 mill tailings, 648 in mines, 570±571 overview, 570±578 plogeny, 570, 577±578 remedial methods, 576±577, 580 toxicity, 351, 567, 572, 579, 656±657 in water, 578±580 Reading Prong, radon levels, 572 Recycling, see also Waste disposal glass, 770±771, 783±784 metal, 770±771, 785±786 motor oil, 153±154 overview, 770, 783 paper, 770±771, 784 plastics, 770±771, 786±791 mixed postconsumer plastics, 788 reuse, 788±789 tertiary recycling, 789±791 tires, 781±782 Redox reactions, in aqueous media, 320±324 Red tide, see Algal blooms Reduction process, metal extraction from ores, 455 Residence times, water systems, 421±422 Resistance, organophosphate insecticides, 274±276, 286 Reverse osmosis, water puri®cation, 438 Risk, 6±7 Rivers composition, 415±417 residence times, 422 Roasting, metal extraction from ores, 455 Rock composition, 443±448 description, 473±474 radioactivity, 565±567, 581 weathering, 461±462, 473±474 Roentgen, unit of exposure to x and gamma radiation, 538±539 Rotenone, resistance, 276

S Salinity, 301, 441 Salt, irrigation water quality, 441 Sandstone, 446

Schumann±Runge bands, 96±97 Sea turtles crude oil effects on marine life, 167±168 plastic refuse effects, 213±214 Sedimentary rock, 446 Selenium biological role, 350, 407±408 drinking water standards, 427 environmental sources, 350, 407 toxicity, 350, 408, 441 Sensitization, photochemical kinetics, 87±88 Serpentine, 446 Sewage sludge, 434±435, 776±777 Shale, 446 Shippingport Nuclear Reactor, 616 Silicon, see also Silicates abundance, 446±447 Silicates asbestos, 444, 477±481 biological role, 349 environmental sources, 349 glass, 475 half-life, 564 ocean composition, 417±420 silicate structures, 447±448 toxicity, 349 Silver biological role, 350 coordination chemistry in aqueous media, 326, 328±329 drinking water standards, 427 environmental sources, 350 recovery from ore, 453 toxicity, 350 Single-photon emission tomography, radiation sources, 597±598 Slate, 446 Small-scale climates, 63±65 Smog, photochemistry characteristics, 3, 126±129, 140±142 nitrogen oxides volatile organic compound absence, 129±135 volatile organic compound presence, 127±129, 135±140 urban atmospheres, 135±140 Soaps biological oxygen demand, 206 microbial metabolism, 201±206 overview, 193±197, 218±219





Sodium abundance, 446 in batteries, 748 biological role, 348 coordination chemistry in aqueous media, 339 decay scheme, 22 Na, 513 environmental sources, 348 half-life 22 Na, 513, 564 24 Na, 564 irrigation water quality, 441 nuclear reaction energetics, 490 ocean composition, 417±418, 420 toxicity, 348 Sodium-cooled, fast breeder reactors, nuclear ®ssion power plants, 615±616 Soil biological effects, 461±462 composition, 460±469 contamination, 469±473 formation, 460±469 isotope fractionation, 584 overview, 460 pro®le, 464 radioactivity, 565±567 types, 467±468 water reactions, 461, 468 weathering, 461±462 Solar energy biological utilization, 711±713 overview, 710±711 photoelectrochemical utilization, 725±728 photovoltaic utilization, 721±727, 738 physical utilization, 713±721 cooling, 713±716 heating, 713±716 ocean thermal energy conversion, 719±720, 738 solar ponds, 717±719 solar thermal power, 716±717, 738 Solar radiation energy balance of the earth, 39±49, 54 photochemical principles, see Photochemistry sunspot cycle, 54 Solar thermal energy, 719±720, 738 Solubility pH effects, 317±319 water environments, 303±306 Spectroscopic states

atoms, 793±796 diatomic molecules, 796±799 overview, 793 polyatomic molecules, 799±800 Spodosols, 467 Stearic acid salts, saponi®cation process, 196±197 Steel, recycling, 770±771 Stefan±Boltzmann law, 40, 44±45 Stone, see Rock Strati®cation carbon dioxide turnover, 305 water properties, 300±301 Stratosphere, see Atmosphere Strobane, resistance, 286 Strontium biological half-life, 550 biological role, 382±383 in consumer products, 600±601 radiostrontium, 90 Sr decay scheme, 512 half-life, 639 in fallout, 632, 653±654, 679 in radioisotope thermoelectric generators, 600±601 in rad waste, 638, 639, 679 toxicity, 382, 632, 653±655 Substitute natural gas, synthesis from coal, 699 Sulfate drinking water standards, 427 in natural anaerobic water systems, 439±440 Sulfur biological role, 349 environmental sources, 349, 370, 372 half-life, 564 sulfur cycle, 370±375 toxicity, 349 Sulfur-containing compounds, see also speci®c compounds atmospheric concentration, 16, 19±20, 373 in internal combustion engines, 173 petroleum combustion, 149±150 redox reactions in aqueous media, 322±323 sulfur cycle, 370±375 volcanic eruptions, 61 Sulfur dioxide air pollution reduction, 172, 374±375 petroleum combustion, 149, 698 sulfur cycle, 370±375 upper atmosphere reactions, 111 Sulfuric acid, see also Acid rain





acid±base reactions, 308 environmental effects, 373±374, 473 Superconductivity, energy storage, 741 Surfactants biological oxygen demand, 206 detergents, 194, 197±198 linear alkylsulfonate synthesis, 198±200 microbial metabolism, 201±206 nonionic alcohol ethoxylate synthesis, 200±201 overview, 193±196, 198, 218±219 Symbols, 807±810 Synchrotron, uses, 602

T Tar sands, petroleum production, 696±697 TCDD, see 2,3,7,8±Tetrachlorodibenzo-pdioxin Technetium, in nuclear medicine, 595±598 Tellurium toxicity, 408 Temperature, see also Global climate changes; Thermal pollution equilibrium effects in aqueous media, 319±320 Temperature inversions, climate effects, 65±69 Terpenes, in air pollution, 171 Terylene, synthesis, 212 Tetraalkylead compounds, in gasoline, 169±170, 177±179, 401 2,3,7,8±Tetrachlorodibenzo-p-dioxin phaseout, 288 toxicity, 236±237, 267±270 Thallium, drinking water standards, 427 Thermal neutron analysis, 602±603 Thermal pollution description, 693 from geothermal energy production, 730, 738 Thermal processes hydrogen fuel cells, 742±743, 750±754 kinetics, 83±87 Thermodynamics laws, 689±693 units of energy and power, 694 Thermonuclear power plants, 624±626 Thiazole, petroleum combustion, 150 Thiophosphoric acid derivatives, synthesis, 271 Thorium average annual exposure, 657 biological half-life, 550 decay series, 801±802

environmental sources, 565±568, 580 half-life, 232 Th, 566, 801 radiometric age determination, 587 Three Mile Island, 665±667, 706 Threshold Test Ban Treaty, 630 Tidal power costs, 739 description, 734±735 Tin biological role, 350, 400±405 environmental sources, 350 recovery from ore, 453 recycling, 770±771, 785 toxicity, 350, 400±401 tributyltin, 400±401 Tires, disposal problems, 781±782 Titanium abundance, 446 biological role, 349 environmental sources, 349 recovery from ore, 453 toxicity, 349 Titanium dioxide in hydrogen production, 728 in paper production, 212 Toxaphene, resistance, 286 Toxicity, see also speci®c substances irrigation water quality, 441 National Toxicology Program, 207, 268 1,1,1-Trichloro-2,2-bis(p-chlorophenyl)ethane action mechanisms, 254±255 analogues, 254±255 dechlorination reaction, 229 environmental degradation, 253±254 overview, 251 related compounds, 255±258 resistance, 274±276, 286 synthesis, 252±253 toxicity, 235±238, 255±258 Trimedlure, insect attractant, 281 2,4,5±Triphenoxyacetic acid environmental degradation, 266±270 overview, 265 synthesis, 265±266 toxicity, 267±270 Tritium atmospheric levels, 569 in consumer products, 599±600 3 H, 564 nuclear fusion, 516±517 unit, 569





Tungsten biological role, 351 environmental sources, 351 recovery from ore, 453 toxicity, 351 x-ray spectrum, 527

U Ultraviolet radiation ozone relationship, 29±30 properties, 77±78, 80 solar emission, 40±44 United Nations Intergovernmental Panel on Climate Change, 13, 355±356 Units of measure, 805±806 Uranium average annual exposure, 657 biological half-life, 550 biological role, 352 in consumer products, 599 decay series, 499±500, 515 depleted, 609, 615, 628±629 environmental sources, 352, 565±568, 580 isotopes 233 U half-life, 518 production, 518 reactor fuel, 609, 614 234 U half-life, 566, 639 235 U enrichment, 628 half-life, 566, 639 in nuclear weapons, 627±628 reactor fuel, 608±609 236 U half-life, 578, 639 238 U decay scheme, 515 half-life, 500, 566, 639 metal, 628 mill tailings, 648±650 neutron induced, 517±521 in nuclear weapons, 627±630, 634±635 radiometric age determination, 586±587, 590 toxicity, 352, 628 Urban areas hydrocarbon sources, 179±182 low-emission automobiles, 181±182

reduction plans, 180±181 microclimates, 63±65 smog photochemistry, 135±140

V Vanadium biological role, 349 environmental sources, 349 half-life, 566 toxicity, 349 Vertisols, 467 Viruses, insect control, 283 Visible light, photochemistry, 75±83 light absorption, 77±83 light properties, 75±77 Volatile organic compounds, see also speci®c compounds in smog, 127±129, 135±140 Volcanic activity atmospheric photochemistry, 111±112 climate change effects, 60±61 ¯uorine compounds, 412 igneous rock, 445 sulfur cycle, 371±375

W Waste disposal, see also Recycling methods anaerobic digestion, 777 composting, 775±777 dilution, 5±6 incineration, 477, 777±781 land®lls, 5, 772±775 nuclear waste, see Nuclear waste ocean disposal, 6 overview, 4±6, 769±772 tires, 781±782 Waste Isolation Pilot Plant, 646±647 Water-cooled, graphite-moderated reactors, 613±614 Water environments acid±base behavior, 306±307 acid±base reactions, 306±319 autoionization, 306±307 carbonic acid, 308, 311±317 overview, 307±311 pH, 310±311, 317±319 solubility, 317±319 adsorption, 341±343 colloidal materials, 340±341 coordination chemistry, 324±340





complexing, 330±339 coordination number, 325±327 description, 324±325, 383±384 geometry, 325±327 metal±ligand preferences, 327±329 water as a ligand, 329±330 ion exchange, 341±343 oxidation±reduction processes, 320±324 temperature and pressure effects, 319±320 solubility, 303±306 water cycle, 295±297 water properties, 298±303 density, 299, 302±303 dissolved salts, 301 freezing, 299 hydrogen bonds, 298±299, 303 ocean currents, 301±302 strati®cation, 300±301 Water pollution, see Pollution Water systems acid rain, 20, 422±425 anaerobic systems, 439±440 composition of water bodies, 415±417 drinking water standards, 426±427 irrigation waters, 440±441 model ocean systems, 417±421 residence times, 421±422 water treatment, 425±438 domestic water treatment, 427±431 chlorination, 429±430 ¯occulating agents, 427±429 ozonolysis, 430±431 wastewater treatment, 432±438 primary sewage treatment, 432±434 secondary sewage treatment, 434±435 tertiary sewage treatment, 435±438 Water vapor atmospheric photochemistry, 125±126 infrared radiation absorption, 45±46 Wave power costs, 739 description, 735±737 Wien's displacement law, 40 Wind energy conversion, 730±733 global circulation, 30±35

overview, 730 production costs, 738 Windscale, nuclear accident, 663±665 World Health Organization arsenic standards, 406 food irradiation, 603, 605

Xenon, atmospheric concentration, 16 X-rays, see also Bremsstrahlung exposure units, 538, 539 focused-beam sources, 593±594 health effects average annual dose, diagnostic, 657±658 deterministic effects, 537±538, 547±548 external sources, 547±549, 655 ionizing radiation, 537±538 stochastic effects, 537±538, 548±549 interactions with matter, 529±533 Compton scattering, 529±531 energy absorption, 530±533 pair production, 530 photoelectric effect, 529 total attenuation, 530±533 properties, 77±78 regulatory limits, 659±661 spectra, tungsten, 527 warning symbol, 66

# Yucca Mountain, 643±644

$ Zeolites description, 446 in detergents, 197 Zero-emission vehicles, 181±182 Zinc in batteries, 749 biological role, 350, 390±399 drinking water standards, 427 environmental sources, 350 recovery from ore, 453 in sewage sludge, 435 toxicity, 350 zircaloy, 609, 613